Changeset 2298

Timestamp:

2010-10-19T17:53:34+02:00 (14 years ago)

Author:

gm

Message:

ticket:#658 add OBS and ASM plus clean of the biblio

Location:

branches/nemo_v3_3_beta/DOC/TexFiles

Files:

• Biblio/Biblio.bib (modified) (176 diffs)
• Chapters/Chap_ASM.tex (added)
• Chapters/Chap_OBS.tex (added)
• Figures/Fig_ASM_obsdist_global.pdf (added)
• Figures/Fig_ASM_obsdist_local.pdf (added)
• Namelist/namasm (added)
• Namelist/namobs (added)
• Namelist/namobs_example (added)
• Namelist/namzdf_gls (moved) (moved from branches/nemo_v3_3_beta/DOC/TexFiles/Namelist/namgls)

branches/nemo_v3_3_beta/DOC/TexFiles/Biblio/Biblio.bib

@@ -104 +104 @@
 @ARTICLE{Arakawa1966,
   author = {A. Arakawa},
-  title = {Computational design for long term numerical integration of the equations of fluid motion, two-dimensional incompressible flow, Part. I.},
+  title = {Computational design for long term numerical integration of the equations 
+    of fluid motion, two-dimensional incompressible flow, Part. I.},
   journal = JCP,
   year = {1966},
@@ -113 +114 @@
 @ARTICLE{Arakawa_Hsu_MWR90,
   author = {A. Arakawa and Y.-J. G. Hsu},
-  title = {Energy Conserving and Potential-Enstrophy Dissipating Schemes for
-   the Shallow Water Equations},
+  title = {Energy Conserving and Potential-Enstrophy Dissipating Schemes for the Shallow Water Equations},
   journal = MWR,
   year = {1990},
-  volume = {118},
+  volume = {118},  number = {10},
   pages = {1960--1969},
-  number = {10},
-  abstract = {To incorporate potential enstrophy dissipation into discrete shallow
-   water equations with no or arbitrarily small energy dissipation,
-   a family of finite-difference schemes have been derived with which
-   potential enstrophy is guaranteed to decrease while energy is conserved
-   (when the mass flux is nondivergent and time is continuous). Among
-   this family of schemes, there is a member that minimizes the spurious
-   impact of infinite potential vorticities associated with infinitesimal
-   fluid depth. The scheme is, therefore, useful for problems in which
-   the free surface may intersect with the lower boundary.},
-  date = {October 01, 1990},
-  owner = {gm},
-  timestamp = {2007.08.05}
 }
 
@@ -140 +127 @@
   journal = MWR,
   year = {1981},
-  volume = {109},
-  pages = {18--36},
-  number = {1},
-  abstract = {To improve the simulation of nonlinear aspects of the flow over steep
-   topography, a potential enstrophy and energy conserving scheme for
-   the shallow water equations is derived. It is pointed out that a
-   family of schemes can conserve total energy for general flow and
-   potential enstrophy for flow with no mass flux divergence. The newly
-   derived scheme is a unique member of this family, that conserves
-   both potential enstrophy and energy for general flow. Comparison
-   by means of numerical experiment with a scheme that conserves (potential)
-   enstrophy for purely horizontal nondivergent flow demonstrated the
-   considerable superiority of the newly derived potential enstrophy
-   and energy conserving scheme, not only in suppressing a spurious
-   energy cascade but also in determining the overall flow regime. The
-   potential enstrophy and energy conserving scheme for a spherical
-   grid is also presented.},
-  date = {January 01, 1981},
-  owner = {gm},
-  timestamp = {2007.08.05}
+  volume = {109},  number = {1},
+  pages = {18--36}
 }
 
@@ -168 +137 @@
   journal = JPO,
   year = {2006},
-  volume = { 36},
+  volume = {36},
   pages = {1502--1522}
 }
@@ -177 +146 @@
   journal = MWR,
   year = {1972},
-  volume = {100},
-  pages = {487--490},
-  number = {6},
-  abstract = {A simple filter for controlling high-frequency computational and physical
-   modes arising in time integrations is proposed. A linear analysis
-   of the filter with leapfrog, implicit, and semi-implicit, differences
-   is made. The filter very quickly removes the computational mode and
-   is also very useful in damping high-frequency physical waves. The
-   stability of the leapfrog scheme is adversely affected when a large
-   filter parameter is used, but the analysis shows that the use of
-   centered differences with frequency filter is still more advantageous
-   than the use of the Euler-backward method. An example of the use
-   of the filter in an actual forecast with the meteorological equations
-   is shown.},
-  date = {June 01, 1972},
-  owner = {gm},
-  timestamp = {2007.08.03}
+  volume = {100},  number = {6},
+  pages = {487--490}
 }
 
@@ -203 +157 @@
   journal = DSR,
   year = {2009},
-  volume = {in press},
-  owner = {gm},
-  timestamp = {2009.08.19}
+  volume = {56},  number = {11},
+  pages = {1942--1954},
+  doi = {10.1016/j.dsr.2009.06.004},
+  url = {http://dx.doi.org/10.1016/j.dsr.2009.06.004}
 }
 
 @ARTICLE{Aumont_al_GBC99,
   author = {O. Aumont and P. Monfray and J. C. Orr and G. Madec and E. Maier-Reimer},
-  title = {Nutrient trapping in the equatorial Pacific: The ocean circulation
-   solution},
+  title = {Nutrient trapping in the equatorial Pacific: The ocean circulation solution},
   journal = GBC,
   year = {1999},
   volume = {13},
-  pages = {351--369},
-  owner = {gm},
-  timestamp = {2009.08.20}
+  pages = {351--369}
 }
 
 @ARTICLE{Aumont_al_CD98,
-  author = {O. Aumont and J.C. Orr and D. Jamous and P. Monfray and O. Marti
-   and G. Madec},
+  author = {O. Aumont and J.C. Orr and D. Jamous and P. Monfray and O. Marti and G. Madec},
   title = {A degradation approach to accelerate simulations to steady state
    in a 3-D tracer transport model of the global ocean},
@@ -228 +179 @@
   year = {1998},
   volume = {14},
-  pages = {101--116},
-  owner = {gm},
-  timestamp = {2009.08.20}
+  pages = {101--116}
 }
 
 @ARTICLE{Axell_JGR02,
   author = {L. B. Axell},
-  title = {Wind-driven internal waves and Langmuir circulations in a numerical
-   ocean model of the southern Baltic Sea},
+  title = {Wind-driven internal waves and Langmuir circulations in a numerical ocean model of the southern Baltic Sea},
   journal = JGR,
   year = {2002},
   volume = {107},
   doi = {10.1029/2001JC000922},
-  owner = {gm},
-  timestamp = {2009.01.16},
   url = {http://dx.doi.org/10.1029/2001JC000922}
 }
@@ -253 +199 @@
   year = {2006},
   volume = {19},
-  pages = {5889–-5902},
-  owner = {gm},
-  timestamp = {2009.08.19}
+  pages = {5889--5902}
 }
 
 @ARTICLE{Barnier_al_OD06,
   author = {B. Barnier and G. Madec and T. Penduff and J.-M. Molines and A.-M.
-   Treguier and J. Le Sommer and A. Beckmann and A. Biastoch and C.
-   Boning and J. Dengg and C. Derval and E. Durand and S. Gulev and
-   E. Remy and C. Talandier and S. Theetten and M. Maltrud and J. McClean
-   and B. De Cuevas},
+   Treguier and J. Le Sommer and A. Beckmann and A. Biastoch and C. Boning 
+   and J. Dengg and C. Derval and E. Durand and S. Gulev and
+   E. Remy and C. Talandier and S. Theetten and M. Maltrud and J. McClean and B. De Cuevas},
   title = {Impact of partial steps and momentum advection schemes in a global
    ocean circulation model at eddy-permitting resolution.},
@@ -271 +214 @@
   pages = {543--567},
   doi = {10.1007/s10236-006-0082-1},
-  owner = {gm},
-  timestamp = {2008.01.25},
   url = {http://dx.doi.org/10.1007/s10236-006-0082-1}
 }
@@ -278 +219 @@
 @INCOLLECTION{Barnier1996,
   author = {B. Barnier and P. Marchesiello and A.P. de Miranda},
-  title = {Modeling the ocean circulation in the South Atlantic: A strategy
-   for dealing with open boundaries},
+  title = {Modeling the ocean circulation in the South Atlantic: A strategy for dealing with open boundaries},
   booktitle = {The South Atlantic: Present and Past Circulation},
   publisher = {Springer-Verlag, Berlin},
@@ -305 +245 @@
    and C. Lévy and Z.X. Li and G. Madec and P. Marquet and O. Marti
    and S. Planton and L. Terray and O. Thual and S. Valcke},
-  title = {Global coupled simulations of climate change due to increased atmospheric
-   CO2 concentration. C. R. Acad. Sci Paris, 326, 677-684.},
+  title = {Global coupled simulations of climate change due to increased atmospheric CO2 concentration},
   journal = {C. R. Acad. Sci Paris},
   year = {1998},
   volume = {326},
-  pages = {677--684},
-  owner = {gm},
-  timestamp = {2009.08.20}
+  pages = {677--684}
 }
 
@@ -321 +258 @@
   journal = {Ocean modelling and parameterization, E. P. Chassignet and J. Verron
    (eds.), NATO Science Series, Kluwer Academic Publishers},
-  year = {1998},
-  owner = {gm},
-  timestamp = {2007.08.04}
+  year = {1998}
 }
 
@@ -333 +268 @@
   year = {1997},
   volume = {27},
-  pages = {581--591},
-  owner = {gm},
-  timestamp = {2007.08.04}
+  pages = {581--591}
 }
 
 @ARTICLE{Beckmann1993,
   author = {A. Beckmann and D. B. Haidvogel},
-  title = {Numerical Simulation of Flow around a Tall Isolated Seamount. Part
-   I - Problem Formulation and Model Accuracy},
+  title = {Numerical Simulation of Flow around a Tall Isolated Seamount. 
+   Part I - Problem Formulation and Model Accuracy},
   journal = JPO,
   year = {1993},
-  volume = {23},
-  pages = {1736--1753},
-  number = {8},
-  abstract = {A sigma coordinate ocean circulation model is employed to study flow
-   trapped to a tall seamount in a periodic f-plane channel. In Part
-   I, errors arising from the pressure gradient formulation in the steep
-   topography/strong stratification limit are examined. To illustrate
-   the error properties, a linearized adiabatic version of the model
-   is considered, both with and without forcing, and starting from a
-   resting state with level isopycnals. The systematic discretization
-   errors from the horizontal pressure gradient terms are shown analytically
-   to increase with steeper topography (relative to a fixed horizontal
-   grid) and for stronger stratification (as measured by the Burger
-   number). For an initially quiescent unforced ocean, the pressure
-   gradient errors produce a spurious oscillating current that, at the
-   end of 10 days, is approximately 1 cm s−1 in amplitude. The
-   period of the spurious oscillation (about 0.5 days) is shown to be
-   a consequence of the particular form of the pressure gradient terms
-   in the sigma coordinate system. With the addition of an alongchannel
-   diurnal forcing, resonantly generated seamount-trapped waves are
-   observed to form. Error levels in these solutions are less than those
-   in the unforced cases; spurious time-mean currents are several orders
-   of magnitude less in amplitude than the resonant propagating waves.
-   However, numerical instability is encountered in a wider range of
-   parameter space. The properties of these resonantly generated waves
-   is explored in detail in Part II of this study. Several new formulations
-   of the pressure gradient terms are tested. Two of the formulations—constructed
-   to have additional conservation properties relative to the traditional
-   form of the pressure gradient terms (conservation of JEBAR and conservation
-   of energy)—are found to have error properties generally similar
-   to those of the traditional formulation. A corrected gradient algorithm,
-   based upon vertical interpolation of the pressure field, has a dramatically
-   reduced error level but a much more restrictive range of stable behavior.},
-  date = {August 01, 1993},
-  owner = {gm},
-  timestamp = {2007.08.03}
+  volume = {23},  number = {8},
+  pages = {1736--1753}
+}
+
+@ARTICLE{Bernie_al_CD07,
+  author = {D. Bernie and E. Guilyardi and G. Madec and J. M. Slingo and S. J. Woolnough},
+  title = {Impact of resolving the diurnal cycle in an ocean--atmosphere GCM. Part 1: a diurnally forced OGCM},
+  journal = CD,
+  year = {2007},
+  volume = {29},  number = {6},
+  pages = {575--590}
 }
 
 @ARTICLE{Bernie_al_CD08,
-  author = {D. Bernie and E. Guilyardi and G. Madec and J. M. Slingo and S. J.
-   Woolnough},
-  title = {Impact of resolving the diurnal cycle in an ocean--atmosphere GCM.
-   Part 2: A diurnally coupled CGCM},
+  author = {D. Bernie and E. Guilyardi and G. Madec and J. M. Slingo and S. J. Woolnough},
+  title = {Impact of resolving the diurnal cycle in an ocean--atmosphere GCM. Part 2: A diurnally coupled CGCM},
   journal = CD,
   year = {2008},
-  volume = {31, 7},
+  volume = {31},  number = {7},
   pages = {909--925},
   doi = {10.1007/s00382-008-0429-z},
-  owner = {gm},
-  timestamp = {2009.08.16},
   url = {http://dx.doi.org/10.1007/s00382-008-0429-z}
-}
-
-@ARTICLE{Bernie_al_CD07,
-  author = {D. Bernie and E. Guilyardi and G. Madec and J. M. Slingo and S. J.
-   Woolnough},
-  title = {Impact of resolving the diurnal cycle in an ocean--atmosphere GCM.
-   Part 1: a diurnally forced OGCM},
-  journal = CD,
-  year = {2007},
-  volume = {29, 6},
-  pages = {575--590},
-  owner = {gm},
-  timestamp = {2009.08.16}
 }
 
@@ -416 +307 @@
   journal = JC,
   year = {2005},
-  volume = {18 (8)},
-  pages = {1190--1200},
-  owner = {gm},
-  timestamp = {2010.09.26}
+  volume = {18},  number = {8},
+  pages = {1190--1200}
 }
 
 @ARTICLE{Bessiere_al_GRL08,
   author = {L. Bessi\'{e}res and G. Madec and F. Lyard},
-  title = {Global Tidal Residual Mean Circulation: Does it Affect a Climate
-   OGCM?},
+  title = {Global Tidal Residual Mean Circulation: Does it Affect a Climate OGCM?},
   journal = GRL,
   year = {2008},
@@ -431 +319 @@
   pages = {L03609},
   doi = {10.1029/2007GL032644},
-  owner = {gm},
-  timestamp = {2009.08.19},
   url = {http://dx.doi.org/10.1029/2007GL032644}
 }
 
 @ARTICLE{Biastoch_al_JC08,
-  author = {A. Biastoch and C. W. Böning and J. Getzlaff and J.-M. Molines and
-   G. Madec},
+  author = {A. Biastoch and C. W. Böning and J. Getzlaff and J.-M. Molines and G. Madec},
   title = {Causes of interannual – decadal variability in the meridional overturning
    circulation of the mid-latitude North Atlantic Ocean},
   journal = JC,
   year = {2008},
-  volume = {21, 24},
+  volume = {21},  number = {24},
   pages = {6599-6615},
   doi = {10.1175/2008JCLI2404.1},
-  owner = {gm},
-  timestamp = {2009.08.19},
   url = {http://dx.doi.org/10.1175/2008JCLI2404.1}
 }
@@ -453 +336 @@
 @ARTICLE{Blanke_al_JPO99,
   author = {B. Blanke and M. Arhan and G. Madec and S. Roche},
-  title = {Warm Water Paths in the Equatorial Atlantic as Diagnosed with a General
-   Circulation Model},
+  title = {Warm Water Paths in the Equatorial Atlantic as Diagnosed with a General Circulation Model},
   journal = JPO,
   year = {1999},
-  volume = {29, 11},
-  pages = {2753-2768},
-  owner = {gm},
-  timestamp = {2008.05.27}
+  volume = {29},  number = {11},
+  pages = {2753-2768}
 }
 
@@ -473 +353 @@
 }
 
-@ARTICLE{blanketal97,
+@ARTICLE{blanke_al_JC97,
   author = {B. Blanke and J. D. Neelin and D. Gutzler},
   title = {Estimating the effect of stochastic wind forcing on ENSO irregularity},
@@ -479 +359 @@
   year = {1997},
   volume = {10},
-  pages = {1473--1486},
-  abstract = {One open question in El Nin˜o–Southern Oscillation (ENSO) simulation
-   and predictability is the role of random
-   
-   forcing by atmospheric variability with short correlation times, on
-   coupled variability with interannual timescales.
-   
-   The discussion of this question requires a quantitative assessment
-   of the stochastic component of the wind stress
-   
-   forcing. Self-consistent estimates of this noise (the stochastic forcing)
-   can be made quite naturally in an empirical
-   
-   atmospheric model that uses a statistical estimate of the relationship
-   between sea surface temperature (SST) and
-   
-   wind stress anomaly patterns as the deterministic feedback between
-   the ocean and the atmosphere. The authors
-   
-   use such an empirical model as the atmospheric component of a hybrid
-   coupled model, coupled to the GFDL
-   
-   ocean general circulation model. The authors define as residual the
-   fraction of the Florida State University wind
-   
-   stress not explained by the empirical atmosphere run from observed
-   SST, and a noise product is constructed by
-   
-   random picks among monthly maps of this residual.
-   
-   The impact of included or excluded noise is assessed with several
-   ensembles of simulations. The model is
-   
-   run in coupled regimes where, in the absence of noise, it is perfectly
-   periodic: in the presence of prescribed
-   
-   seasonal variability, the model is strongly frequency locked on a
-   2-yr period; in annual average conditions it
-   
-   has a somewhat longer inherent ENSO period (30 months). Addition of
-   noise brings an irregular behavior that
-   
-   is considerably richer in spatial patterns as well as in temporal
-   structures. The broadening of the model ENSO
-   
-   spectral peak is roughly comparable to observed. The tendency to frequency
-   lock to subharmonic resonances
-   
-   of the seasonal cycle tends to increase the broadening and to emphasize
-   lower frequencies. An inclination to
-   
-   phase lock to preferred seasons persists even in the presence of noise-induced
-   irregularity. Natural uncoupled
-   
-   atmospheric variability is thus a strong candidate for explaining
-   the observed aperiodicity in ENSO time series.
-   
-   Model–model hindcast experiments also suggest the importance of atmospheric
-   noise in setting limits to ENSO
-   
-   predictability.},
-  pdf = {Blanke_etal_JC97.pdf}
+  pages = {1473--1486}
 }
 
@@ -549 +368 @@
   journal = JPO,
   year = {1997},
-  volume = {27, 6},
-  pages = {1038--1053},
-  owner = {gm},
-  timestamp = {2008.05.27}
+  volume = {27},  number = {6},
+  pages = {1038--1053}
 }
 
@@ -560 +377 @@
   journal = JPO,
   year = {2001},
-  volume = {31, 6},
-  pages = {1623--1632},
-  owner = {gm},
-  timestamp = {2009.08.20}
+  volume = {31},  number = {6},
+  pages = {1623--1632}
 }
 
@@ -571 +386 @@
   journal = GRL,
   year = {2002},
-  volume = {29, 8},
-  pages = {1081--1084},
-  owner = {gm},
-  timestamp = {2009.08.20}
+  volume = {29},  number = {8},
+  pages = {1081--1084}
 }
 
@@ -587 +400 @@
 }
 
+@ARTICLE{Bloom_al_MWR96,
+  author = {S. C. Bloom and L. L. Takacs and A. M. Da Silva and D. Ledvina},
+  title = {Data assimilation using incremental analysis updates},
+  journal = MWR,
+  year = {1996},
+  volume = {124},
+  pages = {1256--1271}
+}
+
 @ARTICLE{Bopp_al_GBC01,
-  author = {L. Bopp and P. Monfray and O. Aumont and J.-L. Dufresne and H. Le
-   Treut and G. Madec and L. Terray and J.C. Orr},
+  author = {L. Bopp and P. Monfray and O. Aumont and J.-L. Dufresne and H. Le Treut 
+    and G. Madec and L. Terray and J.C. Orr},
   title = {Potential impact of climate change on marine export production},
   journal = GBC,
   year = {2001},
-  volume = {15, 1},
-  pages = {81--101},
-  owner = {gm},
-  timestamp = {2009.08.20}
+  volume = {15},  number = {1},
+  pages = {81--101}
 }
 
@@ -605 +425 @@
   journal = MWR,
   year = {1989},
-  volume = {117},
+  volume = {117},  number = {8},
   pages = {1872--1890},
-  number = {8},
-  abstract = {The possibility of extending existing techniques for turbulence parameterization
-   in the planetary boundary layer to attitude, orography-induced turbulence
-   events is examined. Starting from a well-tested scheme, we show that
-   it is possible to generalize the specification method of the length
-   scales, with no deterioration of the scheme performance in the boundary
-   layer. The new scheme is implemented in a two-dimensional version
-   of a limited-area, numerical model used for the simulation of mesobeta-scale
-   atmospheric flows. Three well-known cases of orographically induced
-   turbulence are studied. The comparison with observations and former
-   studies shows a satisfactory behavior of the new scheme.},
-  date = {August 01, 1989},
-  owner = {gm},
-  timestamp = {2007.08.06}
 }
 
@@ -630 +436 @@
   journal = GRL,
   year = {2001},
-  volume = {28, 8},
-  pages = {1603--1606},
-  owner = {gm},
-  timestamp = {2009.08.20}
+  volume = {28},  number = {8},
+  pages = {1603--1606}
 }
 
 @ARTICLE{de_Boyer_Montegut_al_JGR04,
-  author = {C. de Boyer Mont\'{e}gut and G. Madec and A.S. Fischer and A. Lazar
-   and D. Iudicone},
+  author = {C. de Boyer Mont\'{e}gut and G. Madec and A.S. Fischer and A. Lazar and D. Iudicone},
   title = {Mixed layer depth over the global ocean: An examination of profile
    data and a profile-based climatology},
@@ -646 +449 @@
   pages = {C12003},
   doi = {10.1029/2004JC002378},
-  owner = {gm},
-  timestamp = {2009.08.19},
   url = {http://dx.doi.org/10.1029/2004JC002378}
 }
@@ -657 +458 @@
   journal = JC,
   year = {2007},
-  volume = {20 (13)},
-  pages = {3249--3268},
-  owner = {gm},
-  timestamp = {2009.08.19}
+  volume = {20},  number = {13},
+  pages = {3249--3268}
 }
 
@@ -668 +467 @@
   journal = MWR,
   year = {1978},
-  volume = {106},
+  volume = {106},  number = {8},
   pages = {1125--1136},
-  number = {8},
-  month = aug,
-  abstract = {A simple method for integrating the primitive equations is presented
-   which allows for a timestep increment up to twice that of the conventional
-   leapfrog scheme. It consists of a time-averaging operator, which
-   incorporates three consecutive time levels, on the pressure gradient
-   terms in the equations of motion. An attractive feature of the method
-   is its case in programming, since the resulting finite-difference
-   equations can he solved explicitly.Presented here are linear analyses
-   of the method applied to the barotropic and two-layer baroclinic
-   gravity waves. Also presented is an analysis of the method with a
-   time-damping device incorporated, which is an alternative in controlling
-   linearly amplifying computational modes.},
-  owner = {gm},
-  timestamp = {2007.08.05}
 }
 
 @ARTICLE{Bryan1997,
   author = {K. Bryan},
-  title = {A Numerical Method for the Study of the Circulation of the World
-   Ocean},
+  title = {A Numerical Method for the Study of the Circulation of the World Ocean},
   journal = JCP,
   year = {1997},
-  volume = {135, 2},
-  owner = {gm},
-  timestamp = {2007.08.10}
+  volume = {135},  number = {2}
 }
 
@@ -704 +485 @@
   year = {1984},
   volume = {14},
-  owner = {gm},
-  timestamp = {2007.08.10}
+  pages = {666--673}
 }
 
@@ -711 +491 @@
   author = {H. L. Bryden},
   title = {New polynomials for thermal expansion, adiabatic temperature gradient
-   
-   and potential temperature of sea water},
+    and potential temperature of sea water},
   journal = DSR,
   year = {1973},
   volume = {20},
-  pages = {401--408},
-  owner = {gm},
-  timestamp = {2007.08.04}
+  pages = {401--408}
 }
 
@@ -727 +504 @@
   journal = OM,
   year = {2002},
-  volume = {4},
+  volume = {4},  number = {3-4},
   pages = {347--361},
-  number = {3-4},
   doi = {10.1016/S1463-5003(02)00009-4},
-  owner = {gm},
-  timestamp = {2008.11.28},
   url = {http://dx.doi.org/10.1016/S1463-5003(02)00009-4}
 }
@@ -741 +515 @@
   journal = OM,
   year = {2004},
-  volume = {6, 3-4},
-  pages = {221--244},
-  owner = {gm},
-  timestamp = {2007.08.04}
+  volume = {6},  number = {3-4},
+  pages = {221--244}
 }
 
 @ARTICLE{Campin_al_OM08,
-  author = {Jean-Michel Campin and John Marshall and David Ferreira},
+  author = {J.-M. Campin and J. Marshall and D. Ferreira},
   title = {Sea ice-ocean coupling using a rescaled vertical coordinate z*},
   journal = {Ocean Modelling},
   year = {2008},
-  volume = {24},
-  pages = {1 - 14},
-  number = {1-2},
+  volume = {24},  number = {1-2},
+  pages = {1--14},
   doi = {10.1016/j.ocemod.2008.05.005},
-  issn = {1463-5003},
-  timestamp = {2010.01.20},
   url = {http://dx.doi.org/10.1016/j.ocemod.2008.05.005}
 }
 
 @ARTICLE{Campin_Goosse_Tel99,
-  author = {J. M. Campin and H. Goosse},
-  title = {Parameterization of density-driven downsloping flow for a coarse-resolution
-   ocean model in z-coordinate},
+  author = {J.-M. Campin and H. Goosse},
+  title = {Parameterization of density-driven downsloping flow for a coarse-resolution ocean model in z-coordinate},
   journal = {Tellus},
   year = {1999},
   volume = {51},
-  pages = {412--430},
-  owner = {gm},
-  timestamp = {2008.01.20}
+  pages = {412--430}
 }
 
@@ -779 +545 @@
   journal = GRL,
   year = {2003},
-  volume = {30, (6)},
+  volume = {30},  number = {6},
   doi = {10.1029/2002GL016473},
-  owner = {gm},
-  timestamp = {2010.05.21},
   url = {http://dx.doi.org/10.1029/2002GL016473}
 }
@@ -797 +561 @@
   author = {Eric P. Chassignet and Linda T. Smith and George R. Halliwell},
   title = {North Atlantic Simulations with the Hybrid Coordinate Ocean Model
-   (HYCOM): Impact of the Vertical Coordinate Choice, Reference Pressure,
-   and Thermobaricity},
+   (HYCOM): Impact of the Vertical Coordinate Choice, Reference Pressure, and Thermobaricity},
   journal = {Journal of Physical Oceanography},
   year = {2003},
   volume = {33},
-  pages = {2504-2526},
-  timestamp = {2010.02.01}
+  pages = {2504-2526}
 }
 
 @ARTICLE{Covey_al_CD00,
   author = {C. Covey and A. Abe-Ouchi and G.J. Boer and B.A. Boville and U. Cubasch
-   and L. Fairhead and G.M. Flato and H. Gordon and E. Guilyardi and
-   X. Jiang and T.C. Johns and H. Le Treut and G. Madec and G.A. Meehl
-   and R. Miller and A. Noda and S. B. Power and E. Roeckner and G.
-   Russell and E.K. Schneider and R.J. Stouffer and L. Terray and J.-S.
-   von Storch},
-  title = {The seasonal cycle in coupled ocean-atmosphere general circulation
-   models},
+   and L. Fairhead and G.M. Flato and H. Gordon and E. Guilyardi and X. Jiang 
+   and T.C. Johns and H. Le Treut and G. Madec and G.A. Meehl and R. Miller 
+   and A. Noda and S. B. Power and E. Roeckner and G. Russell and E.K. Schneider 
+   and R.J. Stouffer and L. Terray and J.-S. von Storch},
+  title = {The seasonal cycle in coupled ocean-atmosphere general circulation models},
   journal = CD,
   year = {2000},
   volume = {16},
-  pages = {775--787},
-  owner = {gm},
-  timestamp = {2009.08.20}
+  pages = {775--787}
 }
 
@@ -828 +586 @@
   journal = JPO,
   year = {2001},
-  volume = {24, 12},
-  pages = {2546--2559},
-  owner = {gr},
-  timestamp = {2010.09.09}
+  volume = {24},  number = {12},
+  pages = {2546--2559}
 }
 
@@ -840 +596 @@
   year = {1987},
   volume = {74},
-  pages = {1--9},
-  owner = {gm},
-  timestamp = {2007.08.03}
+  pages = {1--9}
 }
 
@@ -850 +604 @@
   journal = JPO,
   year = {1994},
-  volume = {24, 12},
-  pages = {2546--2559},
-  owner = {g5},
-  timestamp = {2010.09.09}
+  volume = {24},  number = {12},
+  pages = {2546--2559}
 }
 
@@ -862 +614 @@
   journal = OM,
   year = {2007},
-  volume = {17, 1},
-  pages = {28--48},
-  owner = {gm},
-  timestamp = {2009.08.19}
-}
-
-@ARTICLE{Dorscher_Beckmann_JAOT00,
-  author = {R. D\"{o}scher and A. Beckmann},
-  title = {Effects of a Bottom Boundary Layer Parameterization in a Coarse-Resolution
-   Model of the North Atlantic Ocean},
-  journal = JAOT,
-  year = {2000},
-  volume = {17},
-  pages = {698--707},
-  owner = {gm},
-  timestamp = {2008.01.23}
+  volume = {17},  number = {1},
+  pages = {28--48}
+}
+
+@BOOK{Daley_Barker_Bk01,
+  author = {R. Daley and E. Barker},
+  title = {NAVDAS Source Book 2001},
+  publisher = {NRL/PU/7530-01-441, Available from the Naval Research Laboratory, Monterey, CA., 93943-5502},
+  year = {2001},
+  pages = {163pp}
 }
 
@@ -887 +633 @@
   year = {2004},
   volume = {304},
-  pages = {390},
-  owner = {gm},
-  timestamp = {2009.08.19}
+  pages = {390}
 }
 
@@ -907 +651 @@
   year = {2008},
   volume = {34},
-  pages = {8--13},
-  owner = {gm},
-  timestamp = {2008.02.03}
+  pages = {8--13}
 }
 
@@ -919 +661 @@
    Eds. W. R. Holland, S. Joussaume and F. David, Elsevier Science},
   year = {2000},
-  pages = {237--313},
-  owner = {gm},
-  timestamp = {2008.02.03}
+  pages = {237--313}
 }
 
@@ -939 +679 @@
   pages = {GB3017},
   doi = {10.1029/2003GB002150},
-  owner = {gm},
-  timestamp = {2009.08.19},
   url = {http://dx.doi.org/10.1029/2003GB002150}
+}
+
+@ARTICLE{Dorscher_Beckmann_JAOT00,
+  author = {R. D\"{o}scher and A. Beckmann},
+  title = {Effects of a Bottom Boundary Layer Parameterization in a Coarse-Resolution
+   Model of the North Atlantic Ocean},
+  journal = JAOT,
+  year = {2000},
+  volume = {17},
+  pages = {698--707}
 }
 
@@ -950 +698 @@
   year = {1994},
   volume = {99},
-  pages = {7991--8014},
-  owner = {gm},
-  timestamp = {2007.08.03}
+  pages = {7991--8014}
 }
 
@@ -962 +708 @@
   journal = JC,
   year = {2007},
-  volume = {20 (10)},
-  pages = {2109--2120},
-  owner = {gm},
-  timestamp = {2009.08.19}
+  volume = {20},  number = {10},
+  pages = {2109--2120}
 }
 
@@ -978 +722 @@
   pages = {L01305},
   doi = {10.1029/2003GL018906},
-  owner = {gm},
-  timestamp = {2009.08.19},
   url = {http://dx.doi.org/10.1029/2003GL018906}
 }
@@ -1005 +747 @@
   year = {2002},
   volume = {4},
-  pages = {89--120},
-  owner = {gm},
-  timestamp = {2009.08.20}
+  pages = {89--120}
 }
 
@@ -1017 +757 @@
   journal = {Environmental Fluid Mechanics},
   year = {2009},
-  volume = {in revision},
-  owner = {gm},
-  timestamp = {2009.08.19}
+  volume = {10},  number = {1-2},
+  pages = {257--273},
+  url = {http://dx.doi.org/10.1007/s10652-009-9159-y}
 }
 
@@ -1026 +766 @@
    and E. M. -Reimer and R. J. Matear and A. Mouchet and I. J. Totterdell
    and Y. Yamanaka and K. Rodgers and G. Madec and J.C. Orr},
-  title = {Evaluation of OCMIP-2 ocean models’ deep circulation
-   
-   with mantle helium-3},
+  title = {Evaluation of OCMIP-2 ocean models’ deep circulation with mantle helium-3},
   journal = JMS,
   year = {2004},
-  pages = {1--22},
-  abstract = {We compare simulations of the injection of mantle helium-3 into the
-   deep ocean from six global coarse resolution models which participated
-   in the Ocean Carbon Model Intercomparison Project (OCMIP). We also
-   discuss the results of a study carried out with one of the models,
-   which examines the effect of the subgrid-scale mixing parameterization.
-   These sensitivity tests provide useful information to interpret the
-   differences among the OCMIP models and between model simulations
-   and the data.
-   
-   We find that the OCMIP models, which parameterize subgrid-scale mixing
-   using an eddy-induced velocity, tend to
-   
-   underestimate the ventilation of the deep ocean, based on diagnostics
-   with d3He. In these models, this parameterization is implemented
-   with a constant thickness diffusivity coefficient. In future simulations,
-   we recommend using such a parameterization with spatially and temporally
-   varying coefficients in order to moderate its effect on stratification.
-   
-   The performance of the models with regard to the formation of AABW
-   confirms the conclusion from a previous evaluation with CFC-11. Models
-   coupled with a sea-ice model produce a substantial bottom water formation
-   in the Southern Ocean that tends to overestimate AABW ventilation,
-   while models that are not coupled with a sea-ice model systematically
-   underestimate the formation of AABW.
-   
-   We also analyze specific features of the deep 3He distribution (3He
-   plumes) that are particularly well depicted in the data and which
-   put severe constraints on the deep circulation. We show that all
-   the models fail to reproduce a correct propagation of these plumes
-   in the deep ocean. The resolution of the models may be too coarse
-   to reproduce the strong and narrow currents in the deep ocean, and
-   the models do not incorporate the geothermal heating that may also
-   contribute to the generation of these currents. We also use the context
-   of OCMIP-2 to explore the potential of mantle helium-3 as a tool
-   to compare and evaluate modeled deep-ocean circulations. Although
-   the source function of mantle helium is known with a rather large
-   uncertainty, we find that the parameterization used for the injection
-   of mantle helium-3 is sufficient to generate realistic results, even
-   in the Atlantic Ocean where a previous pioneering study [J. Geophys.
-   Res. 100 (1995) 3829] claimed this parameterization generates
-   
-   inadequate results. These results are supported by a multi-tracer
-   evaluation performed by considering the simulated distributions of
-   both helium-3 and natural 14C, and comparing the simulated tracer
-   fields with available data.},
-  owner = {sandra},
-  pdf = {Dutay_etal_OCMIP_JMS04.pdf},
-  timestamp = {2006.10.17}
+  pages = {1--22}
 }
 
@@ -1092 +782 @@
   pages = {L12605},
   doi = {10.1029/2005GL022463},
-  owner = {gm},
-  timestamp = {2009.08.19},
   url = {http://dx.doi.org/10.1029/2005GL022463}
 }
@@ -1104 +792 @@
   year = {2001},
   volume = {106},
-  pages = {22475--22502},
-  owner = {gm},
-  timestamp = {2010.05.20}
+  pages = {22475--22502}
 }
 
@@ -1116 +802 @@
   year = {2000},
   volume = {405},
-  pages = {775--778},
-  owner = {gm},
-  timestamp = {2010.05.20}
+  pages = {775--778}
 }
 
@@ -1127 +811 @@
   year = {1980},
   volume = {22},
-  pages = {12--27},
-  owner = {gm},
-  timestamp = {2007.08.03}
+  pages = {12--27}
 }
 
@@ -1138 +820 @@
   year = {2009},
   volume = {5},
-  pages = {281--325},
-  owner = {gm},
-  timestamp = {2008.07.16}
+  pages = {281--325}
 }
 
@@ -1149 +829 @@
  journal = {Tellus},
  volume = {47A},
- pages = {365--382},
+ pages = {365--382}
 }
 
@@ -1155 +835 @@
   author = {EUROMODEL Group (P.M. Lehucher, L. Beautier, M. Chartier, F. Martel,
    L. Mortier, P. Brehmer, C. Millot, C. Alberola, M. Benzhora, I. Taupier-Letage,
-   G. Chabert d'Hieres, H. Didelle, P. Gleizon, D. Obaton, M. Crépon,
+   G. Chabert d'Hieres, H. Didelle, P. Gleizon, D. Obaton, M. Cr\'{e}pon,
    C. Herbaut, G. Madec, S. Speich, J. Nihoul, J. M. Beckers, P. Brasseur,
    E. Deleersnijder, S. Djenidi, J. Font, A. Castellon, E. Garcia-Ladona,
@@ -1166 +846 @@
   title = {EUROMODEL Group (P.M. Lehucher, L. Beautier, M. Chartier, F. Martel,
    L. Mortier, P. Brehmer, C. Millot, C. Alberola, M. Benzhora, I. Taupier-Letage,
-   G. Chabert d'Hieres, H. Didelle, P. Gleizon, D. Obaton, M. Crépon,
+   G. Chabert d'Hieres, H. Didelle, P. Gleizon, D. Obaton, M. Cr\'{e}pon,
    C. Herbaut, G. Madec, S. Speich, J. Nihoul, J. M. Beckers, P. Brasseur,
    E. Deleersnijder, S. Djenidi, J. Font, A. Castellon, E. Garcia-Ladona,
@@ -1176 +856 @@
   journal = {Oceanologica Acta},
   year = {1995},
-  volume = {18, 2},
-  pages = {255--271},
-  owner = {gm},
-  timestamp = {2009.08.20}
+  volume = {18},  number = {2},
+  pages = {255--271}
 }
 
 @PHDTHESIS{Farge1987,
   author = {M. Farge},
-  title = {Dynamique non lineaire des ondes et des tourbillons dans les equations
-   de Saint Venant},
-  school = {Doctorat es Mathematiques, Paris VI University, 401 pp.},
+  title = {Dynamique non lineaire des ondes et des tourbillons dans les equations de Saint Venant},
+  school = {Doctorat es Mathematiques, Paris VI University},
   year = {1987},
-  owner = {gm},
-  timestamp = {2007.08.03}
+  pages = {401pp}
 }
 
@@ -1199 +875 @@
   year = {1995},
   volume = {25},
-  pages = {1731--1741.},
-  owner = {gm},
-  timestamp = {2007.08.04}
+  pages = {1731--1741.}
 }
 
@@ -1229 +903 @@
   year = {1991},
   volume = {96},
-  pages = {759--774},
-  month = jan,
-  owner = {gm},
-  timestamp = {2007.08.04}
+  pages = {759--774}
 }
 
@@ -1241 +912 @@
   year = {1988},
   volume = {45},
-  pages = {55--62},
-  owner = {gr},
-  timestamp = {2010.09.09}
+  pages = {55--62}
 }
 
@@ -1251 +920 @@
   journal = JMR,
   year = {1984},
-  volume = {42},
-  owner = {gm},
-  timestamp = {2007.08.06}
+  volume = {42}
 }
 
 @ARTICLE{Gaspar1990,
   author = {P. Gaspar and Y. Gr{\'e}goris and J.-M. Lefevre},
-  title = {A simple eddy kinetic energy model for simulations of the oceanic
-   vertical mixing\: Tests at Station Papa and long-term upper ocean
-   study site},
+  title = {A simple eddy kinetic energy model for simulations of the oceanic vertical mixing\: 
+    Tests at Station Papa and long-term upper ocean study site},
   journal = JGR,
   year = {1990},
-  volume = {95(C9)},
-  owner = {gm},
-  timestamp = {2007.08.06}
+  volume = {95},  number = {C9}
 }
 
@@ -1273 +937 @@
   journal = JPO,
   year = {1990},
-  volume = {20},
+  volume = {20},  number = {1},
   pages = {150--155},
-  number = {1},
-  abstract = {A subgrid-scale form for mesoscale eddy mixing on isopycnal surfaces
-   is proposed for use in non-eddy-resolving ocean circulation models.
-   The mixing is applied in isopycnal coordinates to isopycnal layer
-   thickness, or inverse density gradient, as well as to passive scalars,
-   temperature and salinity. The transformation of these mixing forms
-   to physical coordinates is also presented.},
-  date = {January 01, 1990},
-  owner = {gm},
-  timestamp = {2007.08.03}
 }
 
@@ -1293 +947 @@
   journal = JGR,
   year = {1993},
-  volume = {98},
-  owner = {gm},
-  timestamp = {2007.08.03}
+  volume = {98}
 }
 
@@ -1305 +957 @@
   year = {1993},
   volume = {98},
-  pages = {14703--14726},
-  owner = {gm},
-  timestamp = {2007.08.03}
+  pages = {14703--14726}
 }
 
@@ -1314 +964 @@
   title = {Standard software development and maintenance},
   institution = {Operational Dep., ECMWF, Reading, UK.},
-  year = {1986},
-  owner = {gm},
-  timestamp = {2008.02.03}
+  year = {1986}
 }
 
@@ -1328 +976 @@
 @ARTICLE{Goosse_al_JGR99,
   author = {H. Goosse and E. Deleersnijder and T. Fichefet and M. England},
-  title = {Sensitivity of a global coupled ocean-sea ice model to the parameterization
-   of vertical mixing},
+  title = {Sensitivity of a global coupled ocean-sea ice model to the parameterization of vertical mixing},
   journal = JGR,
   year = {1999},
   volume = {104},
-  pages = {13,681--13,695},
-  owner = {gm},
-  timestamp = {2008.05.27}
+  pages = {13,681--13,695}
 }
 
 @ARTICLE{Gorgues_al_GRL07,
-  author = {T. Gorgues and C. Menkes and O. Aumont and K. Rodgers and G. Madec
-   and Y. Dandonneau},
-  title = {Indonesian Throughflow control of the eastern equatorial Pacific
-   biogeochemistry},
+  author = {T. Gorgues and C. Menkes and O. Aumont and K. Rodgers and G. Madec and Y. Dandonneau},
+  title = {Indonesian Throughflow control of the eastern equatorial Pacific biogeochemistry},
   journal = GRL,
   year = {2007},
@@ -1348 +991 @@
   pages = {L05609},
   doi = {10.1029/2006GL028210},
-  owner = {gm},
-  timestamp = {2009.08.19},
   url = {http://dx.doi.org/10.1029/2006GL028210}
 }
@@ -1359 +1000 @@
   journal = JGR,
   year = {1994},
-  volume = {99, C6},
-  pages = {12,767--12,771},
-  owner = {gm},
-  timestamp = {2009.10.01}
+  volume = {99},  number = {C6},
+  pages = {12,767--12,771}
 }
 
@@ -1369 +1008 @@
   publisher = {Princeton University Press, 434pp},
   year = {2004},
-  author = {S.M. Griffies},
-  owner = {gm},
-  timestamp = {2007.08.05}
+  author = {S.M. Griffies}
 }
 
@@ -1380 +1017 @@
   year = {1998},
   volume = {28},
-  pages = {831--841},
-  owner = {gm},
-  timestamp = {2008.06.28}
+  pages = {831--841}
 }
 
@@ -1395 +1030 @@
   journal = OM,
   year = {2009},
-  volume = {26, 1-2},
+  volume = {26},  number = {1-2},
   pages = {1--46},
   doi = {10.1016/j.ocemod.2008.08.007},
-  owner = {gm},
-  timestamp = {2009.08.15},
   url = {http://dx.doi.org/}
 }
@@ -1411 +1044 @@
   year = {2005},
   volume = {1},
-  pages = {45--79},
-  abstract = {This paper summarizes the formulation of the ocean component to the
-   Geophysical
-   
-   Fluid Dynamics Laboratory’s (GFDL) coupled climate model used for
-   the 4th IPCC As- Assessment
-   
-   (AR4) of global climate change. In particular, it reviews elements
-   of ocean
-   
-   sessment climate models and how they are pieced together for use in
-   a state-of-the-art coupled 5
-   
-   model. Novel issues are also highlighted, with particular attention
-   given to sensitivity of
-   
-   the coupled simulation to physical parameterizations and numerical
-   methods. Features
-   
-   of the model described here include the following: (1) tripolar grid
-   to resolve the Arctic
-   
-   Ocean without polar filtering, (2) partial bottom step representation
-   of topography to
-   
-   better represent topographically influenced advective and wave processes,
-   (3) more 10
-   
-   accurate equation of state, (4) three-dimensional flux limited tracer
-   advection to reduce
-   
-   overshoots and undershoots, (5) incorporation of regional climatological
-   variability in
-   
-   shortwave penetration, (6) neutral physics parameterization for representation
-   of the
-   
-   pathways of tracer transport, (7) staggered time stepping for tracer
-   conservation and
-   
-   numerical eciency, (8) anisotropic horizontal viscosities for representation
-   of equato- 15
-   
-   rial currents, (9) parameterization of exchange with marginal seas,
-   (10) incorporation
-   
-   of a free surface that accomodates a dynamic ice model and wave propagation,
-   (11)
-   
-   transport of water across the ocean free surface to eliminate unphysical
-   “virtual tracer
-   
-   flux” methods, (12) parameterization of tidal mixing on continental
-   shelves.},
-  owner = {sandra},
-  pdf = {Griffies_al_OSD05.pdf},
-  timestamp = {2007.01.25}
-}
+  pages = {45--79}
+  }
 
 @ARTICLE{Griffies_al_JPO98,
@@ -1476 +1053 @@
   journal = JPO,
   year = {1998},
-  volume = {28},
+  volume = {28},  number = {5},
   pages = {805--830},
-  number = {5},
-  abstract = {This paper considers the requirements that must be satisfied in order
-   to provide a stable and physically based isoneutral tracer diffusion
-   scheme in a z-coordinate ocean model. Two properties are emphasized:
-   1) downgradient orientation of the diffusive fluxes along the neutral
-   directions and 2) zero isoneutral diffusive flux of locally referenced
-   potential density. It is shown that the Cox diffusion scheme does
-   not respect either of these properties, which provides an explanation
-   for the necessity to add a nontrivial background horizontal diffusion
-   to that scheme. A new isoneutral diffusion scheme is proposed that
-   aims to satisfy the stated properties and is found to require no
-   horizontal background diffusion.},
-  date = {May 01, 1998},
-  owner = {gm},
-  timestamp = {2007.08.05}
 }
 
@@ -1501 +1063 @@
   journal = MWR,
   year = {2001},
-  volume = {129},
+  volume = {129},  number = {5},
   pages = {1081--1098},
-  number = {5},
-  abstract = {This paper details a free surface method using an explicit time stepping
-   scheme for use in z-coordinate ocean models. One key property that
-   makes the method especially suitable for climate simulations is its
-   very stable numerical time stepping scheme, which allows for the
-   use of a long density time step, as commonly employed with coarse-resolution
-   rigid-lid models. Additionally, the effects of the undulating free
-   surface height are directly incorporated into the baroclinic momentum
-   and tracer equations. The novel issues related to local and global
-   tracer conservation when allowing for the top cell to undulate are
-   the focus of this work. The method presented here is quasi-conservative
-   locally and globally of tracer when the baroclinic and tracer time
-   steps are equal. Important issues relevant for using this method
-   in regional as well as large-scale climate models are discussed and
-   illustrated, and examples of scaling achieved on parallel computers
-   provided.},
-  date = {May 01, 2001},
-  owner = {gm},
-  timestamp = {2007.08.04}
 }
 
 @ARTICLE{Guilyardi_al_JC04,
-  author = {E. Guilyardi and S. Gualdi and J. M. Slingo and A. Navarra and P.
-   Delecluse and J. Cole and G. Madec and M. Roberts and M. Latif and
-   L. Terray},
-  title = {Representing El Ni\~{n}o in coupled ocean-atmosphere GCMs: the dominant
-   role of the atmospheric component},
+  author = {E. Guilyardi and S. Gualdi and J. M. Slingo and A. Navarra and P. Delecluse 
+    and J. Cole and G. Madec and M. Roberts and M. Latif and L. Terray},
+  title = {Representing El Ni\~{n}o in coupled ocean-atmosphere GCMs: the dominant role of the atmospheric component},
   journal = JC,
   year = {2004},
   volume = {17},
-  pages = {4623--4629},
-  owner = {gm},
-  timestamp = {2009.08.19}
+  pages = {4623--4629}
 }
 
 @ARTICLE{Guilyardi_Madec_CD98,
   author = {E. Guilyardi and G. Madec},
-  title = {Performance of the OPA-ARPEGE-T21 global ocean-atmosphere coupled
-   model},
+  title = {Performance of the OPA-ARPEGE-T21 global ocean-atmosphere coupled model},
   journal = CD,
   year = {1997},
   volume = {13},
-  pages = {149--165},
-  owner = {gm},
-  timestamp = {2009.08.20}
+  pages = {149--165}
 }
 
 @ARTICLE{Guilyardi_al_CD01,
   author = {E. Guilyardi and G. Madec and L. Terray},
-  title = {The role of lateral ocean physics in the upper ocean thermal balance
-   of a coupled ocean-atmosphere GCM},
+  title = {The role of lateral ocean physics in the upper ocean thermal balance of a coupled ocean-atmosphere GCM},
   journal = CD,
   year = {2001},
   volume = {17},
   pages = {589--599},
-  number = {8},
-  pdf = {/home/ericg/TeX/Papers/Published_pdfs/Guilyardi_al_CD01.pdf}
+  number = {8}
 }
 
@@ -1569 +1103 @@
   journal = {C. R. Acad. Sci Paris},
   year = {1995},
-  volume = {320, s\'{e}rie IIa},
-  pages = {683--690},
-  owner = {gm},
-  timestamp = {2009.08.20}
+  volume = {320},  number = {s\'{e}rie IIa},
+  pages = {683--690}
 }
 
@@ -1581 +1113 @@
   year = {1999},
   volume = {Euro-Par'99},
-  pages = {603--607},
-  owner = {gm},
-  timestamp = {2008.05.27}
+  pages = {603--607}
 }
 
@@ -1592 +1122 @@
   journal = {Calculateurs Paralleles},
   year = {1999},
-  volume = {11, 4},
-  pages = {499--517},
-  owner = {gm},
-  timestamp = {2008.05.27}
+  volume = {11},  number = {4},
+  pages = {499--517}
 }
 
 @BOOK{Haltiner1980,
   title = {Numerical prediction and dynamic meteorology},
-  publisher = {John Wiley {\&} Sons Eds., second edition, 477pp},
+  publisher = {John Wiley {\&} Sons Eds., second edition},
   year = {1980},
   author = {G. J. Haltiner and R. T. Williams},
-  owner = {gm},
-  timestamp = {2007.08.03}
+  pages = {477pp}
 }
 
 @ARTICLE{Haney1991,
   author = {R. L. Haney},
-  title = {On the Pressure Gradient Force over Steep Topography in Sigma Coordinate
-   Ocean Models},
+  title = {On the Pressure Gradient Force over Steep Topography in Sigma Coordinate Ocean Models},
   journal = JPO,
   year = {1991},
-  volume = {21},
+  volume = {21},  number = {4},
   pages = {610--619},
-  number = {4},
-  abstract = {The error in computing the pressure gradient force near steep topography
-   using terms following (σ) coordinates is investigated in an
-   ocean model using the family of vertical differencing schemes proposed
-   by Arakawa and Suarez. The truncation error is estimated by substituting
-   known buoyancy profiles into the finite difference hydrostatic and
-   pressure gradient terms. The error due to “hydrostatic inconsistency,”
-   which is not simply a space truncation error, is also documented.
-   The results show that the pressure gradient error is spread throughout
-   the water column, and it is sensitive to the vertical resolution
-   and to the placement of the grid points relative to the vertical
-   structure of the buoyancy field being modeled. Removing a reference
-   state, as suggested for the atmosphere by Gary, reduces the truncation
-   error associated with the two lowest vertical modes by a factor of
-   2 to 3. As an example, the error in computing the pressure gradient
-   using a standard 10-level primitive equation model applied to buoyancy
-   profiles and topographic slopes typical of the California Current
-   region corresponds to a false geostrophic current of the order of
-   10–12 cm s−1. The analogous error in a hydrostatically
-   consistent 30-level model with the reference state removed is about
-   an order of magnitude smaller.},
-  date = {April 01, 1991},
-  owner = {gm},
-  timestamp = {2007.08.03}
 }
 
@@ -1647 +1149 @@
   year = {1974},
   volume = {14},
-  pages = {227-253},
-  owner = {gm},
-  timestamp = {2010.04.14}
+  pages = {227--253}
 }
 
 @ARTICLE{Hofmeister_al_OM09,
-  author = {Richard Hofmeister and Hans Burchard and Jean-Marie Beckers},
+  author = {R. Hofmeister and H. Burchard and J.-M. Beckers},
   title = {Non-uniform adaptive vertical grids for 3D numerical ocean models},
   journal = {Ocean Modelling},
   year = {2009},
   volume = {33},
-  pages = {70 - 86},
+  pages = {70--86},
   doi = {10.1016/j.ocemod.2009.12.003},
-  file = {:Users/mlelod/Documents/Biblio/vertical_coordinates/Hofmeister_et_al_OM_2010.pdf:PDF},
+  url = {http://dx.doi.org/10.1016/j.ocemod.2009.12.003},
   issn = {1463-5003},
-  keywords = {Adaptive non-uniform grid},
-  owner = {mlelod},
-  timestamp = {2010.01.21},
-  url = {http://dx.doi.org/10.1016/j.ocemod.2009.12.003}
 }
 
@@ -1674 +1170 @@
   journal = CD,
   year = {2008},
-  volume = {31, 7--8},
+  volume = {31},  number = {7-8},
   pages = {891--908},
   doi = {10.1007/s00382-008-0416-4},
-  owner = {gm},
-  timestamp = {2009.08.19},
   url = {http://dx.doi.org/10.1007/s00382-008-0416-4}
 }
@@ -1684 +1178 @@
 @ARTICLE{Hsu1990,
   author = {Hsu, Yueh-Jiuan G. and Arakawa, Akio},
-  title = {Numerical Modeling of the Atmosphere with an Isentropic Vertical
-   Coordinate},
+  title = {Numerical Modeling of the Atmosphere with an Isentropic Vertical Coordinate},
   journal = MWR,
   year = {1990},
-  volume = {118},
+  volume = {118},  number = {10},
   pages = {1933--1959},
-  number = {10},
-  abstract = {In constructing a numerical model of the atmosphere, we must choose
-   an appropriate vertical coordinate. Among the various possibilities,
-   isentropic vertical coordinates such as the θ-coordinate seem
-   to have the greatest potential, in spite of the technical difficulties
-   in treating the intersections of coordinate surfaces with the lower
-   boundary. The purpose of this paper is to describe the θ-coordinate
-   model we have developed and to demonstrate its potential through
-   simulating the nonlinear evolution of a baroclinic wave.In the model
-   we have developed, vertical discretization maintains important integral
-   constraints, such as conservation of the angular momentum and total
-   energy. In treating the intersections of coordinate surfaces with
-   the lower boundary, we have followed the massless-layer approach
-   in which the intersecting coordinate surfaces are extended along
-   the boundary by introducing massless layers. Although this approach
-   formally eliminates the intersection problem, it raises other computational
-   problems. Horizontal discretization of the continuity and momentum
-   equations in the model has been carefully designed to overcome these
-   problems.Selected results from a 10-day integration with the 25-layer,
-   β-plane version of the model are presented. It seems that the
-   model can simulate the nonlinear evolution of a baroclinic wave and
-   associated dynamical processes without major computational difficulties.},
-  date = {October 01, 1990},
-  owner = {gm},
-  timestamp = {2007.08.05}
 }
 
@@ -1724 +1192 @@
   year = {1993},
   volume = {23},
-  pages = {2428--2446},
-  owner = {gm},
-  timestamp = {2009.05.01}
+  pages = {2428--2446}
 }
 
 @ARTICLE{Iudicone_al_JPO08b,
   author = {D. Iudicone and G. Madec and B. Blanke and S. Speich},
-  title = {The role of Southern Ocean surface forcings and mixing in the global
-   conveyor},
+  title = {The role of Southern Ocean surface forcings and mixing in the global conveyor},
   journal = JPO,
   year = {2008},
   volume = {38},
-  pages = {1377--1400},
-  owner = {gm},
-  timestamp = {2009.08.19}
+  pages = {1377--1400}
 }
 
@@ -1747 +1210 @@
   year = {2008},
   volume = {38},
-  pages = {1357--1376},
-  owner = {gm},
-  timestamp = {2009.08.19}
+  pages = {1357--1376}
 }
 
 @ARTICLE{Iudicone_al_JPO07,
   author = {D. Iudicone and K. Rodgers and R. Schopp and G. Madec},
-  title = {An Exchange window for the Antarctic Intermediate Water Injection
-   into the South Pacific},
+  title = {An Exchange window for the Antarctic Intermediate Water Injection into the South Pacific},
   journal = JPO,
   year = {2007},
   volume = {37},
-  pages = {31--49},
-  owner = {gm},
-  timestamp = {2009.08.19}
+  pages = {31--49}
 }
 
@@ -1770 +1228 @@
   year = {2008},
   volume = {38},
-  pages = {1401--1425},
-  owner = {gm},
-  timestamp = {2009.08.19}
-}
-
-@ARTICLE{Izumo_al_CD09,
+  pages = {1401--1425}
+}
+
+@ARTICLE{Izumo_al_CD10,
   author = {T. Izumo and S.Masson and J. Vialard and C. de Boyer Montegut and
    S. K. Behera and G. Madec and K. Takahashi and T. Yamagata},
-  title = {Interannual variations of low-frequency Madden-Julian Oscillation
-   in autral summer: Observations},
+  title = {Interannual variations of low-frequency Madden-Julian Oscillation in autral summer: Observations},
   journal = CD,
-  year = {2009},
-  volume = {in press},
-  owner = {gm},
-  timestamp = {2009.08.19}
+  year = {2010},
+  volume = {35},  number = {4},
+  pages = {669--683},
+  url = {http://dx.doi.org/10.1007/s00382-009-0655-z}
 }
 
@@ -1793 +1248 @@
   year = {1995},
   volume = {12},
-  pages = {381--389},
-  owner = {gm},
-  timestamp = {2007.08.04}
+  pages = {381--389}
 }
 
 @ARTICLE{Jayne_St_Laurent_GRL01,
   author = {S.R. Jayne and L.C. {St. Laurent}},
-  title = {Parameterizing tidal disspiation over rough topography
-   
-   .},
+  title = {Parameterizing tidal disspiation over rough topography},
   journal = GRL,
-  pages = {811--814},
-  owner = {gm},
-  timestamp = {2010.05.20}
+  pages = {811--814}
 }
 
@@ -1814 +1263 @@
   year = {1968},
   author = {N. G. Jerlov},
-  pages = {194pp},
-  owner = {gm},
-  timestamp = {2008.08.31}
+  pages = {194pp}
+}
+
+@ARTICLE{Jones_MWR99,
+  author = {P. W. Jones},
+  title = {First- and second-order conservative remapping schemes for grids in spherical coordinates},
+  journal = MWR,
+  year = {1999},
+  volume = {127},
+  pages = {2204--2210}
+}
+
+@BOOK{Jones_Bk01,
+  title = {A User's Guide for SCRIP: A Spherical Coordinate Remapping and Interpolation Package. Version 1.4},
+  publisher = {Los Alamos National Laboratory},
+  year = {2001},
+  author = {P. W. Jones},
+  pages = {27pp},
+  url = {http://climate.lanl.gov/Software/SCRIP/SCRIPusers.pdf}
 }
 
@@ -1825 +1290 @@
   year = {1994},
   volume = {99},
-  pages = {25,235--25,266},
-  owner = {gr},
-  timestamp = {2010.09.09}
+  pages = {25,235--25,266}
 }
 
@@ -1836 +1299 @@
   year = {2005},
   volume = {61},
-  pages = {693--702},
-  owner = {gm},
-  timestamp = {2010.09.09}
+  pages = {693--702}
 }
 
@@ -1847 +1308 @@
   year = {1974},
   volume = {102},
-  pages = {509--522},
-  owner = {gm},
-  timestamp = {2010.04.14}
+  pages = {509--522}
 }
 
@@ -1857 +1316 @@
   journal = JPO,
   year = {1991},
-  volume = {21},
-  pages = {1333--1348},
-  number = {9},
-  abstract = {A version of the Bryan–Cox–Semtner numerical ocean general
-   circulation model, adapted to include a free surface, is described.
-   The model is designed for the following uses: tidal studies
-   (a tidal option is explicitly included); assimilation of altimetric
-   data (since the surface elevation is now a prognostic variable);
-   and in situations where accurate relaxation to obtain the streamfunction
-   in the original model is too time consuming. Comparison is made between
-   a 300-year run of the original model and the free-surface version,
-   using a very coarse North Atlantic calculation as the basis. The
-   results are very similar, differing only in the streamfunction over
-   topography; this is to be expected, since the treatment of topographic
-   torques on the barotropic flow differs because of the nature of the
-   modifications.},
-  date = {September 01, 1991},
-  owner = {gm},
-  timestamp = {2007.08.03}
+  volume = {21},  number = {9},
+  pages = {1333--1348}
 }
 
@@ -1885 +1327 @@
   editor = {Hawaiian winter workshop},
   month = {January 17-20},
-  organization = {University of Hawaii at Manoa},
-  owner = {gm},
-  timestamp = {2007.08.06}
+  organization = {University of Hawaii at Manoa}
 }
 
@@ -1900 +1340 @@
 
 @ARTICLE{Koch-Larrouy_al_CD10,
-  author = {A. Koch-Larrouy and M. Lengaigne and P. Terray and G. Madec and S.
-   Masson},
-  title = {Tidal mixing in the Indonesian Seas and its effect on the tropical
-   climate system},
+  author = {A. Koch-Larrouy and M. Lengaigne and P. Terray and G. Madec and S. Masson},
+  title = {Tidal mixing in the Indonesian Seas and its effect on the tropical climate system},
   journal = CD,
   year = {2010},
-  volume = {34,6},
+  volume = {34},  number = {6},
   pages = {891--904},
   doi = {10.1007/s00382-009-0642-4},
-  owner = {gm},
-  timestamp = {2009.08.16},
   url = {http://dx.doi.org/10.1007/s00382-009-0642-4}
 }
@@ -1916 +1352 @@
 @ARTICLE{Koch-Larrouy_al_OD08b,
   author = {A. Koch-Larrouy and G. Madec and B. Blanke and R. Molcard},
-  title = {Water mass transformation along the Indonesian throughflow in an
-   OGCM},
+  title = {Water mass transformation along the Indonesian throughflow in an OGCM},
   journal = OD,
   year = {2008},
-  volume = {58, 3-4},
+  volume = {58},  number = {3-4},
   pages = {289--309},
   doi = {10.1007/s10236-008-0155-4},
-  owner = {gm},
-  timestamp = {2009.08.16},
   url = {http://dx.doi.org/10.1007/s10236-008-0155-4}
 }
 
 @ARTICLE{Koch-Larrouy_al_GRL07,
-  author = {A. Koch-Larrouy and G. Madec and P. Bouruet-Aubertot and T. Gerkema
-   and L. Bessieres and R. Molcard},
-  title = {Tidal mixing in the Indonesian Seas and its effect on the tropical
-   climate system},
+  author = {A. Koch-Larrouy and G. Madec and P. Bouruet-Aubertot and T. Gerkema and L. Bessieres and R. Molcard},
+  title = {Tidal mixing in the Indonesian Seas and its effect on the tropical climate system},
   journal = GRL,
   year = {2007},
@@ -1938 +1369 @@
   pages = {L04604},
   doi = {10.1029/2006GL028405},
-  owner = {gm},
-  timestamp = {2009.08.16},
   url = {http://dx.doi.org/10.1029/2006GL028405}
 }
 
 @ARTICLE{Koch-Larrouy_al_OD08a,
-  author = {A. Koch-Larrouy and G. Madec and D. Iudicone and A. Atmadipoera and
-   R. Molcard},
-  title = {Physical processes contributing to the water mass transformation
-   of the Indonesian Throughflow},
+  author = {A. Koch-Larrouy and G. Madec and D. Iudicone and A. Atmadipoera and R. Molcard},
+  title = {Physical processes contributing to the water mass transformation of the Indonesian Throughflow},
   journal = OD,
   year = {2008},
-  volume = {58, 3-4},
+  volume = {58},  number = {3-4},
   pages = {275--288},
   doi = {10.1007/s10236-008-0154-5},
-  owner = {gm},
-  timestamp = {2009.08.16},
   url = {http://dx.doi.org/10.1007/s10236-008-0154-5}
 }
@@ -1964 +1389 @@
   year = {1942},
   volume = {6},
-  pages = {56--58},
-  owner = {gm},
-  timestamp = {2007.08.06}
+  pages = {56--58}
 }
 
@@ -1974 +1397 @@
    nord-occidentale. Cycle saisonnier et variabilit\'{e} m\'{e}so\'{e}chelle},
   school = {Universit\'{e} Pierre et Marie Curie, Paris, France, 207pp},
-  year = {1996},
-  owner = {gm},
-  timestamp = {2007.08.04}
+  year = {1996}
 }
 
@@ -1984 +1405 @@
   journal = GRL,
   year = {2001},
-  volume = {28},
-  owner = {gm},
-  timestamp = {2007.08.04}
-}
-
-@ARTICLE{Levy_al_JGR09,
+  volume = {28}
+}
+
+@ARTICLE{Levy_al_JGR10,
   author = {M. L\'{e}vy and P. Klein and A.-M. Tr\'{e}guier and D. Iovino and
    G. Madec and S. Masson and T. Takahashi},
   title = {Impacts of sub-mesoscale physics on idealized gyres},
   journal = JGR,
-  year = {2009},
-  volume = {in revision},
-  owner = {gm},
-  timestamp = {2009.08.19}
+  year = {2010},
+  volume = {34},  number = {1-2},
+  doi = {10.1016/j.ocemod.2010.04.001},
+  url = {http://dx.doi.org/10.1016/j.ocemod.2010.04.001}
 }
 
@@ -2007 +1426 @@
   journal = JMS,
   year = {1999},
-  volume = {16/1-2},
-  pages = {7--21},
-  owner = {gm},
-  timestamp = {2007.08.10}
+  volume = {16},  number = {1-2},
+  pages = {7--21}
 }
 
@@ -2019 +1436 @@
   journal = DSR,
   year = {1998},
-  volume = {I, 46},
-  pages = {1137--1160},
-  owner = {gm},
-  timestamp = {2007.08.10}
+  volume = {I},  number = {46},
+  pages = {1137--1160}
 }
 
@@ -2032 +1447 @@
   year = {2000},
   volume = {47},
-  pages = {527--531},
-  owner = {gm},
-  timestamp = {2009.08.20}
+  pages = {527--531}
 }
 
 @BOOK{Large_Yeager_Rep04,
-  title = {Diurnal to decadal global forcing for ocean and sea-ice models: the
-   data sets and flux climatologies},
-  publisher = {NCAR Technical Note, NCAR/TN-460+STR, CGD Division of the National
-   Center for Atmospheric Research},
+  title = {Diurnal to decadal global forcing for ocean and sea-ice models: the data sets and flux climatologies},
+  publisher = {NCAR Technical Note, NCAR/TN-460+STR, CGD Division of the National Center for Atmospheric Research},
   year = {2004},
-  author = {W. Large and S. Yeager},
-  owner = {gm},
-  timestamp = {2007.08.06}
-}
+  author = {W. Large and S. Yeager}}
 
 @ARTICLE{Large_al_RG94,
   author = {W. G. Large and J. C. McWilliams and S. C. Doney},
-  title = {Oceanic vertical mixing - a review and a model with a nonlocal boundary
-   layer parameterization},
+  title = {Oceanic vertical mixing - a review and a model with a nonlocal boundary layer parameterization},
   journal = {Reviews of Geophysics},
   year = {1994},
@@ -2057 +1464 @@
   pages = {363--404},
   doi = {10.1029/94RG01872},
-  owner = {gm},
-  timestamp = {2007.08.03},
   url = {http://dx.doi.org/10.1029/94RG01872}
 }
@@ -2069 +1474 @@
   year = {2006},
   volume = {19},
-  pages = {4631--4637},
-  owner = {gm},
-  timestamp = {2009.08.19}
+  pages = {4631--4637}
 }
 
@@ -2080 +1483 @@
    id\'{e}alis\'{e}e},
   school = {Universit\'{e} Pierre et Marie Curie, Paris, France, 200pp},
-  year = {1997},
-  owner = {gm},
-  timestamp = {2007.08.06}
+  year = {1997}
 }
 
@@ -2091 +1492 @@
   journal = JPO,
   year = {1999},
-  volume = {29},
+  volume = {29},  number = {11},
   pages = {2945--2961},
-  number = {11},
-  abstract = {Numerous numerical simulations of basin-scale ocean circulation display
-   a vast interior downwelling and a companion intense western boundary
-   layer upwelling at midlatitude below the thermocline. These features,
-   related to the so-called Veronis effect, are poorly rationalized
-   and depart strongly from the classical vision of the deep circulation
-   where upwelling is considered to occur in the interior. Furthermore,
-   they significantly alter results of ocean general circulation models
-   (OGCMs) using horizontal Laplacian diffusion. Recently, some studies
-   showed that the parameterization for mesoscale eddy effects formulated
-   by Gent and McWilliams allows integral quantities like the streamfunction
-   and meridional heat transport to be free of these undesired effects.
-   In this paper, an idealized OGCM is used to validate an analytical
-   rationalization of the processes at work and help understand the
-   physics. The results show that the features associated with the Veronis
-   effect can be related quantitatively to three different width scales
-   that characterize the baroclinic structure of the deep western boundary
-   current. In addition, since one of these scales may be smaller than
-   the Munk barotropic layer, usually considered to determine the minimum
-   resolution and horizontal viscosity for numerical models, the authors
-   recommend that it be taken into account. Regarding the introduction
-   of the new parameterization, diagnostics in terms of heat balances
-   underline some interesting similarities between local heat fluxes
-   by eddy-induced velocities and horizontal diffusion at low and midlatitudes
-   when a common large diffusivity (here 2000 m2 s−1) is used.
-   The near-quasigeostrophic character of the flow explains these results.
-   As a consequence, the response of the Eulerian-mean circulation is
-   locally similar for runs using either of the two parameterizations.
-   However, it is shown that the advective nature of the eddy-induced
-   heat fluxes results in a very different effective circulation, which
-   is the one felt by tracers.},
-  date = {November 01, 1999},
-  owner = {gm},
-  timestamp = {2007.08.06}
 }
 
@@ -2136 +1503 @@
   journal = OM,
   year = {2009},
-  volume = {29, 1},
+  volume = {29},  number = {1},
   pages = {1--14},
   doi = {10.1016/j.ocemod.2008.11.007},
-  owner = {gm},
-  timestamp = {2009.08.16},
   url = {http://dx.doi.org/10.1016/j.ocemod.2008.11.007}
 }
@@ -2149 +1514 @@
    Eul\'{e}rienne dans le code NEMO, 180pp.},
   school = {Universit\'{e} Pierre and Marie Curie},
-  year = {2010},
-  owner = {gm},
-  timestamp = {2010.09.25}
+  year = {2010}
 }
 
@@ -2159 +1522 @@
   journal = OM,
   year = {2009},
-  volume = {30, 2-3},
+  volume = {30},  number = {2-3},
   pages = {88-94},
   doi = {10.1016/j.ocemod.2009.06.006},
-  owner = {gm},
-  timestamp = {2009.08.15},
   url = {http://dx.doi.org/}
 }
@@ -2174 +1535 @@
   journal = JC,
   year = {2003},
-  volume = {16, 20},
-  pages = {3330--3343},
-  owner = {gm},
-  timestamp = {2009.08.20}
+  volume = {16},  number = {20},
+  pages = {3330--3343}
 }
 
@@ -2187 +1546 @@
   year = {2002},
   doi = {10.1029/2001JC000841},
-  owner = {gm},
-  timestamp = {2009.08.20},
   url = {http://dx.doi.org/10.1029/2001JC000841}
 }
@@ -2198 +1555 @@
   journal = JGR,
   year = {2003},
-  volume = {108 (C11)},
+  volume = {108},  number = {C11},
   pages = {3345},
   doi = {10.1029/2002JC001704},
-  owner = {gm},
-  timestamp = {2008.01.26},
   url = {http://dx.doi.org/10.1029/2002JC001704}
 }
 
 @ARTICLE{Lengaigne_al_GRL09,
-  author = {M. Lengaigne and G. Madec and L. Bopp and C. Menkes and O. Aumont
-   and P. Cadule},
-  title = {Bio-physical feedbacks in the Arctic Ocean using an Earth System
-   model},
+  author = {M. Lengaigne and G. Madec and L. Bopp and C. Menkes and O. Aumont and P. Cadule},
+  title = {Bio-physical feedbacks in the Arctic Ocean using an Earth System model},
   journal = GRL,
   year = {2009},
-  volume = {submitted},
-  owner = {gm},
-  timestamp = {2009.08.19}
+  volume = {36},  
+  pages = {L21602},
+  doi = {10.1029/2009GL040145},
+  url = {http://dx.doi.org/10.1029/2009GL040145}
 }
 
 @ARTICLE{Lengaigne_al_CD07,
-  author = {M. Lengaigne and C. Menkes and O. Aumont and T. Gorgues and L. Bopp
-   and J.-M. Andr\'{e} G. Madec},
+  author = {M. Lengaigne and C. Menkes and O. Aumont and T. Gorgues and L. Bopp and J.-M. Andr\'{e} G. Madec},
   title = {Bio-physical feedbacks on the tropical Pacific climate in a Coupled
    General Circulation Model},
@@ -2226 +1579 @@
   year = {2007},
   volume = {28},
-  pages = {503--516},
-  owner = {gm},
-  timestamp = {2009.08.19}
+  pages = {503--516}
 }
 
 @ARTICLE{Leonard1991,
   author = {B. P. Leonard},
-  title = {The ULTIMATE conservative difference scheme applied to unsteady one--dimensional
-   advection},
+  title = {The ULTIMATE conservative difference scheme applied to unsteady one--dimensional advection},
   journal = {Computer Methods in Applied Mechanics and Engineering},
   year = {1991},
-  pages = {17--74},
-  owner = {gm},
-  timestamp = {2007.08.04}
+  pages = {17--74}
 }
 
 @TECHREPORT{Leonard_Rep88,
   author = {B. P. Leonard},
-  title = {Universal limiter for transient interpolation modelling of the advective
-   transport equations},
+  title = {Universal limiter for transient interpolation modelling of the advective transport equations},
   institution = {Technical Memorandum TM-100916 ICOMP-88-11, NASA},
-  year = {1988},
-  owner = {gm},
-  timestamp = {2007.08.04}
+  year = {1988}
 }
 
@@ -2260 +1605 @@
   volume = {19},
   pages = {59--98},
-  month = jun,
-  owner = {gm},
-  timestamp = {2007.08.04}
 }
 
@@ -2270 +1612 @@
   institution = {MERSEA MERSEA IP report WP09-CNRS-STR-03-1A, 47pp, available on the
    NEMO web site},
-  year = {2007},
-  owner = {gm},
-  timestamp = {2007.08.03}
+  year = {2007}
 }
 
@@ -2280 +1620 @@
   year = {1982},
   author = {S Levitus },
-  note = {173 p.}
+  pages = {173 pp}
 }
 
@@ -2289 +1629 @@
   institution = {LODYC, France, 36pp.},
   year = {1989},
-  number = {3},
-  owner = {gm},
-  timestamp = {2007.08.03}
+  number = {3}
 }
 
@@ -2300 +1638 @@
   year = {1990},
   volume = {88},
-  pages = {1--4},
-  owner = {gm},
-  timestamp = {2007.08.03}
+  pages = {1--4}
 }
 
@@ -2311 +1647 @@
   journal = JC,
   year = {2005},
-  volume = {18 (13)},
-  pages = {2344--2360},
-  owner = {gm},
-  timestamp = {2009.08.19}
+  volume = {18},  number = {13},
+  pages = {2344--2360}
 }
 
@@ -2322 +1656 @@
    (IPSL), France, No 27, ISSN No 1288-1619},
   year = {2008},
-  author = {G. Madec},
-  owner = {gm},
-  timestamp = {2008.07.05}
+  author = {G. Madec}
 }
 
 @BOOK{Madec_HDR01,
-  title = {Le Cycle des Masses d'Eau Oc\'{e}aniqueset sa variabilit\'{e} dans
-   le Syst\'{e}me Climatique},
+  title = {Le Cycle des Masses d'Eau Oc\'{e}aniqueset sa variabilit\'{e} dans le Syst\'{e}me Climatique},
   year = {2001},
   author = {G. Madec},
   pages = {63pp.},
-  series = {Habilitation \'{a} Diriger des Recherches, Universit\'{e} Pierre
-   et Marie Curie},
-  owner = {gm},
-  timestamp = {2009.08.20}
+  series = {Habilitation \'{a} Diriger des Recherches, Universit\'{e} Pierre et Marie Curie}
 }
 
@@ -2345 +1673 @@
   school = {Universit\'{e} Pierre et Marie Curie, Paris, France, 194pp.},
   year = {1990},
-  month = {2 mai},
-  owner = {gm},
-  timestamp = {2007.08.10}
+  month = {2 mai}
 }
 
@@ -2358 +1684 @@
   year = {1991},
   volume = {15},
-  pages = {301--332},
-  owner = {gm},
-  timestamp = {2007.08.06}
+  pages = {301--332}
 }
 
 @ARTICLE{Madec_al_JPO91,
   author = {G. Madec and M. Chartier and P. Delecluse and M. Cr\'{e}pon},
-  title = {A three-dimensional numerical study of deep water formation in the
-   
-   
-   Northwestern Mediterranean Sea .},
+  title = {A three-dimensional numerical study of deep water formation in the Northwestern Mediterranean Sea .},
   journal = JPO,
   year = {1991},
   volume = {21},
-  pages = {1349--1371},
-  owner = {gm},
-  timestamp = {2007.08.06}
+  pages = {1349--1371}
 }
 
@@ -2384 +1703 @@
   publisher = {Elsevier Oceanographic Series, P.C. Chu and J.C. Gascard (Eds.)},
   year = {1991},
-  author = {G. Madec and M. Cr\'{e}pon},
-  owner = {gm},
-  timestamp = {2007.08.06}
-}
+  author = {G. Madec and M. Cr\'{e}pon}
+  }
 
 @ARTICLE{Madec1997,
@@ -2395 +1712 @@
   year = {1997},
   volume = {26},
-  pages = {12--15},
-  owner = {gm},
-  timestamp = {2007.08.06}
+  pages = {12--15}
 }
 
@@ -2422 +1737 @@
   journal = JPO,
   year = {1996},
-  volume = {26},
+  volume = {26},  number = {8},
   pages = {1393--1408},
-  number = {8},
-  month = aug,
-  abstract = {The large-scale processes preconditioning the winter deep-water formation
-   in the northwestern Mediterranean Sea are investigated with a primitive
-   equation numerical model where convection is parameterized by a non-penetrative
-   convective adjustment algorithm. The ocean is forced by momentum
-   and buoyancy fluxes that have the gross features of mean winter forcing
-   found in the MEDOC area. The wind-driven barotropic circulation appears
-   to be a major ingredient of the preconditioning phase of deep-water
-   formation. After three months, the ocean response is dominated by
-   a strong barotropic cyclonic vortex located under the forcing area,
-   which fits the Sverdrup balance away from the northern coast. In
-   the vortex center, the whole water column remains trapped under the
-   forcing area all winter. This trapping enables the thermohaline forcing
-   to drive deep-water formation efficiently. Sensitivity studies show
-   that, β effect and bottom topography play a paramount role and
-   confirm that deep convection occurs only in areas that combine a
-   strong surface thermohaline forcing and a weak barotropic advection
-   so that water masses are submitted to the negative buoyancy fluxes
-   for a much longer time. In particular, the impact of the Rhône
-   Deep Sea Fan on the barotropic circulation dominates the β effect:
-   the barotropic flow is constrained to follow the bathymetric contours
-   and the cyclonic vortex is shifted southward so that the fluid above
-   the fan remains quiescent. Hence, buoyancy fluxes trigger deep convection
-   above the fan in agreement with observations. The selection of the
-   area of deep-water formation through the defection of the barotropic
-   circulation by the topography seems a more efficient mechanism than
-   those associated with the wind- driven barotropic vortex. This is
-   due to its permanency, while the latter may be too sensitive to time
-   and space variations of the forcing.},
-  owner = {gm},
-  timestamp = {2007.08.03}
 }
 
@@ -2465 +1748 @@
   year = {1988},
   volume = {78},
-  pages = {1-6},
-  owner = {gm},
-  timestamp = {2009.08.20}
+  pages = {1-6}
 }
 
@@ -2477 +1758 @@
   year = {1998},
   volume = {14},
-  pages = {55--70},
-  owner = {gm},
-  timestamp = {2009.08.20}
+  pages = {55--70}
 }
 
@@ -2487 +1766 @@
   journal = MWR,
   year = {1997},
-  volume = {125, 5},
-  pages = {958--971},
-  owner = {gm},
-  timestamp = {2009.08.20}
+  volume = {125},  number = {5},
+  pages = {958--971}
 }
 
@@ -2499 +1776 @@
   journal = JGR,
   year = {1998},
-  volume = {103(C13)},
-  pages = {30,825--30,854},
-  owner = {gm},
-  timestamp = {2007.08.05}
+  volume = {103},  number = {C13},
+  pages = {30,825--30,854}
 }
 
@@ -2522 +1797 @@
   journal = OM,
   year = {2008},
-  volume = {20},
+  volume = {20},  number = {1},
   pages = {61--89},
-  number = {1},
   doi = {10.1016/j.ocemod.2007.07.005},
-  owner = {gm},
-  timestamp = {2008.11.28},
   url = {http://dx.doi.org/10.1016/j.ocemod.2007.07.005}
 }
@@ -2538 +1810 @@
    Molod and S. Dutkiewicz and H. Hill and M. Losch and B. Fox-Kemper
    and D. Menemenlis and D. Ferreira and E. Hill and M. Follows and
-   C. Hill and C. Evangelinos and G. Forget},
-  owner = {gm},
-  timestamp = {2008.07.04}
-}
+   C. Hill and C. Evangelinos and G. Forget}
+   }
 
 @PHDTHESIS{Marti_PhD92,
@@ -2548 +1818 @@
    et du transport de traceurs anthropog\'{e}niques},
   school = {Universit\'{e} Pierre et Marie Curie, Paris, France, 201pp},
-  year = {1992},
-  owner = {gm},
-  timestamp = {2007.08.04}
-}
-
-@ARTICLE{Marti_al_CD09,
+  year = {1992}
+}
+
+@ARTICLE{Marti_al_CD10,
   author = {O. Marti and P. Braconnot and J.-L. Dufresne and J. Bellier and R.
    Benshila and S. Bony and P. Brockmann and P. Cadule and A. Caubel
@@ -2564 +1832 @@
    to atmospheric resolution},
   journal = CD,
-  year = {2009},
-  volume = {in press},
-  owner = {gm},
-  timestamp = {2009.08.19}
+  year = {2010},
+  volume = {34},  number = {1},
+  pages = {1--26},
+  doi = {10.1007/s00382-009-0640-6},
+  url = {http://dx.doi.org/10.1007/s00382-009-0640-6}
 }
 
@@ -2577 +1846 @@
   year = {1992},
   volume = {97},
-  pages = {12,763--12,766},
-  month = aug,
-  owner = {gm},
-  timestamp = {2007.08.03}
+  pages = {12,763--12,766}
 }
 
@@ -2591 +1857 @@
   year = {2008},
   editor = {Resch M, Roller S, Lammers P, Furui T, Galle M, Bez W},
-  author = {S. Masson and M.-A. Foujols and P. Klein and G. Madec and L. Hua
-   and M. Levy and H. Sasaki and K. Takahashi and F. Svensson},
+  author = {S. Masson and M.-A. Foujols and P. Klein and G. Madec and L. Hua and M. Levy 
+  and H. Sasaki and K. Takahashi and F. Svensson},
   doi = {10.1007/978-3-540-74384-2},
-  owner = {gm},
-  timestamp = {2009.08.19},
   url = {http://dx.doi.org/10.1007/978-3-540-74384-2}
 }
@@ -2610 +1874 @@
   pages = {L07703},
   doi = {10.1029/2004GL021980},
-  owner = {gm},
-  timestamp = {2009.08.19},
   url = {http://dx.doi.org/10.1029/2004GL021980}
 }
@@ -2620 +1882 @@
   journal = JPO,
   year = {1987},
-  volume = {17},
+  volume = {17},  number = {11},
   pages = {1950--1964},
-  number = {11},
-  abstract = {Scalar properties in the ocean are stirred (and subsequently mixed)
-   rather efficiently by mesoscale eddies and two-dimensional turbulence
-   along “neutral surfaces”, defined such that when water
-   parcels are moved small distances in the neutral surface, they experience
-   no buoyant restoring forces. By contrast, work would have to be done
-   on a moving fluid parcel in order to keep it on a potential density
-   surface. The differences between neutral surfaces and potential density
-   surfaces are due to the variation of α/β with pressure
-   (where α is the thermal expansion coefficient and β is
-   the saline contraction coefficient). By regarding the equation of
-   state of seawater as a function of salinity, potential temperature,
-   and pressure, rather than in terms of salinity, temperature, and
-   pressure, it is possible to quantify the differences between neutral
-   surfaces and potential density surfaces. In particular, the spatial
-   gradients of scalar properties (e.g., S, θ, tritium or potential
-   vorticity) on a neutral surface can be quite different to the corresponding
-   gradients in a potential density surface. For example, at a potential
-   temperature of 4°C and a pressure of 1000 db, the lateral gradient
-   of potential temperature in a potential density surface (referenced
-   to sea level) is too large by between 50% and 350% (depending
-   on the stability ratio Rp of the water column) compared with the
-   physically relevant gradient of potential temperature on the neutral
-   surface. Three-examples of neutral surfaces are presented, based
-   on the Levitus atlas of the North Atlantic.},
-  date = {November 01, 1987},
-  owner = {gm},
-  timestamp = {2007.08.04}
 }
 
 @ARTICLE{McDougall_Taylor_JMR84,
   author = {T. J. McDougall and J. R. Taylor},
-  title = {Flux measurements across a finger interface at low values of the
-   stability ratio},
+  title = {Flux measurements across a finger interface at low values of the stability ratio},
   journal = JMR,
   year = {1984},
   volume = {42},
-  pages = {1--14},
-  owner = {gm},
-  timestamp = {2008.05.20}
+  pages = {1--14}
 }
 
@@ -2670 +1901 @@
   year = {2004},
   volume = {34},
-  pages = {693--698},
-  owner = {gm},
-  timestamp = {2009.01.16}
+  pages = {693--698}
 }
 
@@ -2681 +1910 @@
   year = {1982},
   volume = {20},
-  pages = {851-875},
-  owner = {gr},
-  timestamp = {2010.09.09}
+  pages = {851--875}
 }
 
 @ARTICLE{Menkes_al_JPO06,
-  author = {C. Menkes and J. Vialard and S C. Kennan and J.-P. Boulanger and
-   G. Madec},
+  author = {C. Menkes and J. Vialard and S C. Kennan and J.-P. Boulanger and G. Madec},
   title = {A modelling study of the three-dimensional heat budget of Tropical
-   Instability Waves in the Equatorial Pacific},
+    Instability Waves in the Equatorial Pacific},
   journal = JPO,
   year = {2006},
-  volume = {36, 5},
-  pages = {847--865},
-  owner = {gm},
-  timestamp = {2009.08.19}
+  volume = {36},  number = {5},
+  pages = {847--865}
 }
 
@@ -2704 +1928 @@
   journal = JPO,
   year = {1999},
-  volume = {29},
-  pages = {1124--1142},
-  number = {6},
-  abstract = {A global ocean model is described in which parameterizations of diapycnal
-   mixing by double-diffusive fingering and layering are added to a
-   stability-dependent background turbulent diffusivity. Model runs
-   with and without double-diffusive mixing are compared for annual-mean
-   and seasonally varying surface forcing. Sensitivity to different
-   double-diffusive mixing parameterizations is considered. In all cases,
-   the locales and extent of salt fingering (as diagnosed from buoyancy
-   ratio Rρ) are grossly comparable to climatology, although fingering
-   in the models tends to be less intense than observed. Double-diffusive
-   mixing leads to relatively minor changes in circulation but exerts
-   significant regional influences on temperature and salinity.},
-  date = {June 01, 1999},
-  owner = {gm},
-  timestamp = {2007.08.06}
+  volume = {29},  number = {6},
+  pages = {1124--1142}
 }
 
@@ -2727 +1936 @@
   publisher = {GARP Publication Series No 17},
   year = {1976},
-  author = {F. Mesinger and A. Arakawa},
-  owner = {gm},
-  timestamp = {2008.02.09}
+  author = {F. Mesinger and A. Arakawa}
 }
 
 @ARTICLE{Morel_JGR88,
   author = {A. Morel},
-  title = {Optical modeling of the upper ocean in relation to its biogenous
-   matter content (Case I waters)},
+  title = {Optical modeling of the upper ocean in relation to its biogenous matter content (Case I waters)},
   journal = JGR,
   year = {1988},
   volume = {93},
-  pages = {10,749--10,768},
-  owner = {gm},
-  timestamp = {2010.10.07}
+  pages = {10,749--10,768}
 }
 
@@ -2749 +1953 @@
   journal = JGR,
   year = {2001},
-  owner = {gm},
-  timestamp = {2010.10.07}
+  volume = {106}, number = {C4},
+  pages = {7163--7180}
 }
 
 @ARTICLE{Moun_al_JPO02,
   author = {J.N. Moum and D.R. Caldwell and J.D. Nash and G.D. Gunderson},
-  title = {Observations of boundary mixing over the 
-   
-   continental slope},
-  journal = JPO,
-  owner = {gm},
-  timestamp = {2010.05.20}
+  title = {Observations of boundary mixing over the continental slope},
+  journal = JPO,
+  year = {2002},
+  volume = {32}, number = {7},
+  pages = {2113--2130}
 }
 
@@ -2768 +1971 @@
   journal = JCP,
   year = {1996},
-  volume = {126},
+  volume = {126},  number = {2},
   pages = {251--273},
-  number = {2},
-  month = {July},
-  owner = {gm},
-  timestamp = {2007.08.03}
 }
 
@@ -2781 +1980 @@
    dans un jet g\'{e}ostrophique: le front Alm\'{e}ria-Oran},
   school = {Universit\'{e} Pierre et Marie Curie, Paris, France},
-  year = {2001},
-  owner = {gm},
-  timestamp = {2007.08.14}
+  year = {2001}
 }
 
 @ARTICLE{Osborn_JPO80,
   author = {T.R. Osborn},
-  title = {Estimates of the local rate of vertical diffusion from dissipation
-   measurements},
+  title = {Estimates of the local rate of vertical diffusion from dissipation measurements},
   journal = JPO,
   volume = {10},
-  pages = {83--89},
-  owner = {gm},
-  timestamp = {2010.05.20}
+  pages = {83--89}
 }
 
 @ARTICLE{Pacanowski_Philander_JPO81,
   author = {R.C. Pacanowski and S.G.H. Philander},
-  title = {Parameterization of Vertical Mixing in Numerical Models of Tropical
-   Oceans},
+  title = {Parameterization of Vertical Mixing in Numerical Models of Tropical Oceans},
   journal = JPO,
   year = {1981},
-  volume = {11},
-  pages = {1443--1451},
-  number = {11},
-  abstract = {Measurements indicate that mixing processes are intense in the surface
-   layers of the ocean but weak below the thermocline, except for the
-   region below the core of the Equatorial Undercurrent where vertical
-   temperature gradients are small and the shear is large. Parameterization
-   of these mixing processes by means of coefficients of eddy mixing
-   that are Richardson-number dependent, leads to realistic simulations
-   of the response of the equatorial oceans to different windstress
-   patterns. In the case of eastward winds results agree well with measurements
-   in the Indian Ocean. In the case of westward winds it is of paramount
-   importance that the nonzero heat flux into the ocean be taken into
-   account. This beat flux stabilizes the upper layers and reduces the
-   intensity of the mixing, especially in the cast. With an appropriate
-   surface boundary condition, the results are relatively insensitive
-   to values assigned to constants in the parameterization formula.},
-  date = {November 01, 1981},
-  owner = {gm},
-  timestamp = {2007.08.03}
+  volume = {11},  number = {11},
+  pages = {1443--1451}
 }
 
 @ARTICLE{Pacanowski_Gnanadesikan_MWR98,
   author = {R. C. Pacanowski and A. Gnanadesikan},
-  title = {Transient response in a z-level ocean model that resolves topography
-   
-   
-   with partial-cells},
+  title = {Transient response in a z-level ocean model that resolves topography with partial-cells},
   journal = MWR,
   year = {1998},
   volume = {126},
-  pages = {3248-3270},
-  owner = {gm},
-  timestamp = {2008.01.26}
+  pages = {3248--3270}
 }
 
 @ARTICLE{Park_al_JC09,
-  author = {W. Park and N. Keenlyside and M. Latif and A. Str\¨{o}h and R. Redler
-   and E. Roeckner and G. Madec},
+  author = {W. Park and N. Keenlyside and M. Latif and A. Str\¨{o}h and R. Redler and E. Roeckner and G. Madec},
   title = {Tropical Pacific Climate and its Response to Global Warming in the
    Kiel Climate Model},
   journal = JC,
   year = {2009},
-  volume = {22, 1},
+  volume = {22},  number = {1},
   pages = {71--92},
   doi = {10.1175/2008JCLI2261.1},
-  owner = {gm},
-  timestamp = {2009.08.19},
   url = {http://dx.doi.org/10.1175/2008JCLI2261.1}
 }
@@ -2859 +2026 @@
   journal = JPO,
   year = {1977},
-  volume = {7},
-  pages = {952--956},
-  number = {6},
-  abstract = {Observations were made of downward solar radiation as a function of
-   depth during an experiment in the North Pacific (35°N, 155°W).
-   The irradiance meter employed was sensitive to solar radiation of
-   wavelength 400–1000 nm arriving from above at a horizontal
-   surface. Because of selective absorption of the short and long wavelengths,
-   the irradiance decreases much faster than exponential in the upper
-   few meters, falling to one-third of the incident value between 2
-   and 3 m depth. Below 10 m the decrease was exponential at a rate
-   characteristic of moderately clear water of Type IA. Neglecting one
-   case having low sun altitude, the observations are well represented
-   by the expression I/I0=Rez/ζ1+(1−R)ezζ2,
-   where I is the irradiance at depth −z, I0 is the irradiance
-   at the surface less reflected solar radiation, R=0.62, ζ1
-   and ζ2 are attenuation lengths equal to 1.5 and 20 m, respectively,
-   and z is the vertical space coordinate, positive upward with the
-   origin at mean sea level. The depth at which the irradiance falls
-   to 10% of its surface value is nearly the same as observations
-   of Secchi depth when cases with high wind speed or low solar altitude
-   are neglected. Parameters R, ζ1, and ζ2 are computed for
-   the entire range of oceanic water types.},
-  date = {November 01, 1977},
-  owner = {gm},
-  timestamp = {2007.08.04}
+  volume = {7},  number = {6},
+  pages = {952--956}
 }
 
 @ARTICLE{Penduff_al_OM06,
   author = {T. Penduff and B. Barnier and J.-M. Molines and G. Madec},
-  title = {On the use of current meter data to assess the realism of ocean model
-   simulations},
+  title = {On the use of current meter data to assess the realism of ocean model simulations},
   journal = OM,
   year = {2006},
-  volume = {11, 3--4},
-  pages = {399--416},
-  owner = {gm},
-  timestamp = {2009.08.19}
+  volume = {11},  number = {3--4},
+  pages = {399--416}
 }
 
 @ARTICLE{Penduff_al_JGR00,
   author = {T. Penduff and B. Barnier and A. Colin de Verdi\`{e}re},
-  title = {Self-adapting open boundaries for a regional model of the eastern
-   North Atlantic},
+  title = {Self-adapting open boundaries for a regional model of the eastern North Atlantic},
   journal = JGR,
   year = {2000},
@@ -2910 +2049 @@
 
 @ARTICLE{Penduff_al_OS07,
-  author = {T. Penduff and J. Le Sommer and B. Barnier and A.M. Treguier and
-   J. Molines and G. Madec},
+  author = {T. Penduff and J. Le Sommer and B. Barnier and A.M. Treguier and J. Molines and G. Madec},
   title = {Influence of numerical schemes on current-topography interactions
    in 1/4$^{\circ}$ global ocean simulations},
@@ -2922 +2060 @@
 @ARTICLE{Phillips1959,
   author = {R. S. Phillips},
-  title = {Dissipative Operators and Hyperbolic Systems of Partial Differential
-   Equations},
+  title = {Dissipative Operators and Hyperbolic Systems of Partial Differential Equations},
   journal = {Transactions of the American Mathematical Society},
   year = {1959},
-  volume = {90 (2)},
+  volume = {90},  number = {2},
   pages = {193--254},
   doi = {10.2307/1993202},
-  owner = {gm},
-  timestamp = {2007.08.10},
   url = {http://dx.doi.org/10.2307/1993202}
 }
 
 @ARTICLE{Le_Quere_al_GBC00,
-  author = {C. Le Qu\'{e}r\'{e} and J. C. Orr and P. Monfray and O. Aumont and
-   G. Madec},
-  title = {Interannual variability of the global and regional sea-air flux of
-   C02 from 1979 to 1993},
+  author = {C. Le Qu\'{e}r\'{e} and J. C. Orr and P. Monfray and O. Aumont and G. Madec},
+  title = {Interannual variability of the global and regional sea-air flux of C02 from 1979 to 1993},
   journal = GBC,
   year = {2000},
   volume = {14},
-  pages = {1247--1266},
-  owner = {gm},
-  timestamp = {2009.08.20}
+  pages = {1247--1266}
 }
 
 @ARTICLE{Raynaud_al_GRL00,
   author = {S. Raynaud and S. Speich and E. Guilyardi and G. Madec},
-  title = {Impact of the ocean lateral diffusion on the ENSO-like variability
-   of a global coupled GCM},
+  title = {Impact of the ocean lateral diffusion on the ENSO-like variability of a global coupled GCM},
   journal = GRL,
   year = {2000},
-  volume = {27, 19},
-  pages = {3041--3044},
-  owner = {gm},
-  timestamp = {2009.08.20}
+  volume = {27},  number = {19},
+  pages = {3041--3044}
 }
 
@@ -2965 +2093 @@
   year = {1982},
   volume = {13},
-  pages = {1154--1158},
-  owner = {gm},
-  timestamp = {2008.02.02}
+  pages = {1154--1158}
 }
 
 @ARTICLE{Reverdin1991,
-  author = {G. Reverdin and P. Delecluse and C. L\'{e}vy and P. Andrich and A.
-   Morli\`{e}re and J. M. Verstraete},
-  title = {The near surface tropical Atlantic in 1982-1984 : results from a
-   numerical simulation and a data analysis},
+  author = {G. Reverdin and P. Delecluse and C. L\'{e}vy and P. Andrich and A. Morli\`{e}re and J. M. Verstraete},
+  title = {The near surface tropical Atlantic in 1982-1984 : results from a numerical simulation and a data analysis},
   journal = PO,
   year = {1991},
   volume = {27},
-  pages = {273-340},
-  owner = {gm},
-  timestamp = {2007.08.04}
+  pages = {273--340}
 }
 
 @BOOK{Richtmyer1967,
   title = {Difference methods for initial-value problems},
-  publisher = {Interscience Publisher, Second Edition, 405pp},
+  publisher = {Interscience Publisher, Second Edition},
   year = {1967},
   author = {R. D. Richtmyer and K. W. Morton},
-  owner = {gm},
-  timestamp = {2007.08.04}
+  pages = {405pp}
 }
 
 @ARTICLE{Robert_JMSJ66,
   author = {A. J. Robert},
-  title = {The integration of a Low order spectral form of the primitive meteorological
-   equations},
+  title = {The integration of a Low order spectral form of the primitive meteorological equations},
   journal = JMSJ,
   year = {1966},
-  volume = {44, 2},
-  owner = {gm},
-  timestamp = {2007.08.04}
+  volume = {44},  number = {2}
 }
 
@@ -3011 +2129 @@
   pages = {L14314},
   doi = {10.1029/2004GL019764},
-  owner = {gm},
-  timestamp = {2009.08.19},
   url = {http://dx.doi.org/10.1029/2004GL019764}
 }
 
 @ARTICLE{Rodgers_al_GRL03,
-  author = {K. Rodgers and B. Blanke and G. Madec and O. Aumont and P. Ciais
-   and J.-C. Dutay},
+  author = {K. Rodgers and B. Blanke and G. Madec and O. Aumont and P. Ciais and J.-C. Dutay},
   title = {Extratropical sources of equatorial pacific upwelling in an OGCM},
   journal = GRL,
   year = {2003},
-  volume = {30, 2},
+  volume = {30},  number = {2},
   doi = {10.1029/2002GL016003},
-  owner = {gm},
-  timestamp = {2009.08.20},
   url = {http://dx.doi.org/10.1029/2002GL016003}
 }
@@ -3034 +2147 @@
   journal = JGR,
   year = {1987},
-  volume = {92, C5},
-  pages = {5305--5328},
-  owner = {gr},
-  timestamp = {2010.09.09}
+  volume = {92},  number = {C5},
+  pages = {5305--5328}
 }
 
@@ -3056 +2167 @@
   year = {2000},
   volume = {105},
-  pages = {23,927--23,942},
-  owner = {gm},
-  pdf = {Roullet_Madec_JGR00.pdf},
-  timestamp = {2007.03.22}
+  pages = {23,927--23,942}
 }
 
@@ -3067 +2175 @@
   journal = JAS,
   year = {1975},
-  volume = {32},
+  volume = {32},  number = {4},
   pages = {680--689},
-  number = {4},
-  abstract = {Two simple numerical models of the shallow-water equations identical
-   in all respects but for their con-servation properties have been
-   tested regarding their internal mixing processes. The experiments
-   show that violation of enstrophy conservation results in a spurious
-   accumulation of rotational energy in the smaller scales, reflected
-   by an unrealistic increase of enstrophy, which ultimately produces
-   a finite rate of energy dissipation in the zero viscosity limit,
-   thus violating the well-known dynamics of two-dimensional flow. Further,
-   the experiments show a tendency to equipartition of the kinetic energy
-   of the divergent part of the flow in the inviscid limit, suggesting
-   the possibility of a divergent energy cascade in the physical system,
-   as well as a possible influence of the energy mixing on the process
-   of adjustment toward balanced flow.},
-  date = {April 01, 1975},
-  owner = {gm},
-  timestamp = {2007.08.05}
 }
 
@@ -3094 +2185 @@
   year = {1982},
   volume = {87},
-  pages = {394--409},
-  owner = {gm},
-  timestamp = {2007.08.04}
+  pages = {394--409}
 }
 
@@ -3105 +2194 @@
   journal = {Ocean Modelling},
   year = {2005},
-  volume = {9, 4},
-  pages = {347--404},
-  owner = {gm},
-  timestamp = {2007.08.04}
+  volume = {9},  number = {4},
+  pages = {347--404}
 }
 
@@ -3114 +2201 @@
   author = {A. F. Shchepetkin and J. C. McWilliams},
   title = {A method for computing horizontal pressure-gradient force in an oceanic
-   model with a nonaligned 
-   
-   vertical coordinate},
+   model with a nonaligned vertical coordinate},
   journal = JGR,
   year = {2003},
-  volume = {108(C3)},
+  volume = {108},  number = {C3},
   pages = {3090},
   doi = {10.1029/2001JC001047},
-  owner = {gm},
-  timestamp = {2007.08.05},
   url = {http://dx.doi.org/10.1029/2001JC001047}
 }
@@ -3129 +2212 @@
 @ARTICLE{Shchepetkin1996,
   author = {A. F. Shchepetkin and J. J. O'Brien},
-  title = {A Physically Consistent Formulation of Lateral Friction in Shallow-Water
-   Equation Ocean Models},
+  title = {A Physically Consistent Formulation of Lateral Friction in Shallow-Water Equation Ocean Models},
   journal = MWR,
   year = {1996},
-  volume = {124},
-  pages = {1285--1300},
-  number = {6},
-  abstract = {Dissipation in numerical ocean models has two purposes: to simulate
-   processes in which the friction is physically relevant and to prevent
-   numerical instability by suppressing accumulation of energy in the
-   smallest resolved scales. This study shows that even for the latter
-   case the form of the friction term should be chosen in a physically
-   consistent way. Violation of fundamental physical principles reduces
-   the fidelity of the numerical solution, even if the friction is small.
-   Several forms of the lateral friction, commonly used in numerical
-   ocean models, are discussed in the context of shallow-water equations
-   with nonuniform layer thickness. It is shown that in a numerical
-   model tuned for the minimal dissipation, the improper form of the
-   friction term creates finite artificial vorticity sources that do
-   not vanish with increased resolution, even if the viscous coefficient
-   is reduced consistently with resolution. An alternative numerical
-   implementation of the no-slip boundary conditions for an arbitrary
-   coast line is considered. It was found that the quality of the numerical
-   solution may be considerably improved by discretization of the viscous
-   stress tensor in such a way that the numerical boundary scheme approximates
-   not only the stress tensor to a certain order of accuracy but also
-   simulates the truncation error of the numerical scheme used in the
-   interior of the domain. This ensures error cancellation during subsequent
-   use of the elements of the tensor in the discrete version of the
-   momentum equations, allowing for approximation of them without decrease
-   in the order of accuracy near the boundary.},
-  date = {June 01, 1996},
-  owner = {gm},
-  timestamp = {2007.08.14}
+  volume = {124},  number = {6},
+  pages = {1285--1300}
 }
 
@@ -3171 +2225 @@
   year = {2004},
   pages = {245--263},
-  abstract = {Astronomical data reveals that approximately 3.5 terawatts (TW) of
-   tidal energy is dissipated in the
-   
-   ocean. Tidal models and satellite altimetry suggest that 1 TW of this
-   energy is converted from the barotropic
-   
-   to internal tides in the deep ocean, predominantly around regions
-   of rough topography such as midocean
-   
-   ridges. Aglobal tidal model is used to compute turbulent energy levels
-   associated with the dissipation
-   
-   of internal tides, and the diapycnal mixing supported by this energy
-   ?ux is computed using a simple parameterization.
-   
-   The mixing parameterization has been incorporated into a coarse resolution
-   numerical model of the
-   
-   global ocean. This parameterization o?ers an energetically consistent
-   and practical means of improving the
-   
-   representation of ocean mixing processes in climate models. Novel
-   features of this implementation are that
-   
-   the model explicitly accounts for the tidal energy source for mixing,
-   and that the mixing evolves both
-   
-   spatially and temporally with the model state. At equilibrium, the
-   globally averaged di?usivity pro?le
-   
-   ranges from 0.3 cm2 s
-   abyss with a depth average of 0.9
-   
-   cm2 s
-   Water properties are strongly in?uenced
-   
-   by the combination of weak mixing in the main thermocline and enhanced
-   mixing in the deep ocean.
-   
-   Climatological comparisons show that the parameterized mixing scheme
-   results in a substantial reduction},
-  owner = {gm},
-  pdf = {Simmons_mixing_OM2003.pdf},
-  timestamp = {2007.03.22}
 }
 
 @ARTICLE{Song_Haidvogel_JCP94,
   author = {Y. Song and D. Haidvogel},
-  title = {A semi-implicit ocean circulation model using a generalized topography-following
-   coordinate system},
+  title = {A semi-implicit ocean circulation model using a generalized topography-following coordinate system},
   journal = JCP,
   year = {1994},
-  volume = {115, 1},
-  pages = {228--244},
-  owner = {gm},
-  timestamp = {2007.08.04}
+  volume = {115},  number = {1},
+  pages = {228--244}
 }
 
 @ARTICLE{Song1998,
   author = {Y. T. Song},
-  title = {A General Pressure Gradient Formulation for Ocean Models. Part I:
-   Scheme Design and Diagnostic Analysis},
+  title = {A General Pressure Gradient Formulation for Ocean Models. Part I: Scheme Design and Diagnostic Analysis},
   journal = MWR,
   year = {1998},
-  volume = {126},
-  pages = {3213--3230},
-  number = {12},
-  abstract = {A Jacobian formulation of the pressure gradient force for use in models
-   with topography-following coordinates is proposed. It can be used
-   in conjunction with any vertical coordinate system and is easily
-   implemented. Vertical variations in the pressure gradient are expressed
-   in terms of a vertical integral of the Jacobian of density and depth
-   with respect to the vertical computational coordinate. Finite difference
-   approximations are made on the density field, consistent with piecewise
-   linear and continuous fields, and accurate pressure gradients are
-   obtained by vertically integrating the discrete Jacobian from sea
-   surface.Two discrete schemes are derived and examined in detail:
-   the first using standard centered differencing in the generalized
-   vertical coordinate and the second using a vertical weighting such
-   that the finite differences are centered with respect to the Cartesian
-   z coordinate. Both schemes achieve second-order accuracy for any
-   vertical coordinate system and are significantly more accurate than
-   conventional schemes based on estimating the pressure gradients by
-   finite differencing a previously determined pressure field.The standard
-   Jacobian formulation is constructed to give exact pressure gradient
-   results, independent of the bottom topography, if the buoyancy field
-   varies bilinearly with horizontal position, x, and the generalized
-   vertical coordinate, s, over each grid cell. Similarly, the weighted
-   Jacobian scheme is designed to achieve exact results, when the buoyancy
-   field varies linearly with z and arbitrarily with x, that is, b(x,z)
-   = b0(x) + b1(x)z.When horizontal resolution cannot be made
-   fine enough to avoid hydrostatic inconsistency, errors can be substantially
-   reduced by the choice of an appropriate vertical coordinate. Tests
-   with horizontally uniform, vertically varying, and with horizontally
-   and vertically varying buoyancy fields show that the standard Jacobian
-   formulation achieves superior results when the condition for hydrostatic
-   consistency is satisfied, but when coarse horizontal resolution causes
-   this condition to be strongly violated, the weighted Jacobian may
-   give superior results.},
-  date = {December 01, 1998},
-  owner = {gm},
-  timestamp = {2007.08.05}
+  volume = {126},  number = {12},
+  pages = {3213--3230}
 }
 
 @ARTICLE{SongWright1998,
   author = {Y. T. Song and D. G. Wright},
-  title = {A General Pressure Gradient Formulation for Ocean Models. Part II
-   - Energy, Momentum, and Bottom Torque Consistency},
+  title = {A General Pressure Gradient Formulation for Ocean Models. 
+    Part II: Energy, Momentum, and Bottom Torque Consistency},
   journal = MWR,
   year = {1998},
-  volume = {126},
-  pages = {3231--3247},
-  number = {12},
-  abstract = {A new formulation of the pressure gradient force for use in models
-   with topography-following coordinates is proposed and diagnostically
-   analyzed in Part I. Here, it is shown that important properties of
-   the continuous equations are retained by the resulting numerical
-   schemes, and their performance in prognostic simulations is examined.
-   Numerical consistency is investigated with respect to global energy
-   conservation, depth-integrated momentum changes, and the representation
-   of the bottom pressure torque. The performances of the numerical
-   schemes are tested in prognostic integrations of an ocean model to
-   demonstrate numerical accuracy and long-term integral stability.
-   Two typical geometries, an isolated tall seamount and an unforced
-   basin with sloping boundaries, are considered for the special case
-   of no external forcing and horizontal isopycnals to test numerical
-   accuracy. These test problems confirm that the proposed schemes yield
-   accurate approximations to the pressure gradient force. Integral
-   consistency conditions are verified and the energetics of the “advective
-   elimination” of the pressure gradient error (Mellor et al)
-   is considered.A large-scale wind-driven basin with and without topography
-   is used to test the model’s long-term integral performance
-   and the effects of bottom pressure torque on the transport in western
-   boundary currents. Integrations are carried out for 10 years in each
-   case and results show that the schemes are stable, and the steep
-   topography causes no obvious numerical problems. A realistic meandering
-   western boundary current is well developed with detached cold cyclonic
-   and warm anticyclonic eddies as it extends across the basin. In addition,
-   the results with topography show earlier separation and enhanced
-   transport in the western boundary currents due to the bottom pressure
-   torque.},
-  date = {December 01, 1998},
-  owner = {gm},
-  timestamp = {2007.08.05}
+  volume = {126},  number = {12},
+  pages = {3231--3247}
 }
 
 @ARTICLE{Speer_al_Tel00,
   author = {K. Speer and E. Guilyardi and G. Madec},
-  title = {Southern Ocean transformation in a coupled model with and without
-   eddy mass fluxes},
+  title = {Southern Ocean transformation in a coupled model with and without eddy mass fluxes},
   journal = {Tellus},
   year = {2000},
-  volume = {52A, 5},
-  pages = {554--565},
-  owner = {gm},
-  timestamp = {2009.08.20}
+  volume = {52A},  number = {5},
+  pages = {554--565}
 }
 
@@ -3334 +2269 @@
    par les d\'{e}troits - cas de la mer d'Alboran},
   school = {Universit\'{e} Pierre et Marie Curie, Paris, France},
-  year = {1992},
-  owner = {gm},
-  timestamp = {2007.08.06}
+  year = {1992}
 }
 
@@ -3344 +2277 @@
   journal = GRL,
   year = {2001},
-  volume = {28, 2},
-  pages = {311--314},
-  owner = {gm},
-  timestamp = {2009.08.20}
+  volume = {28},  number = {2},
+  pages = {311--314}
 }
 
@@ -3355 +2286 @@
   journal = JPO,
   year = {1996},
-  volume = {26, 3},
-  pages = {320--340},
-  owner = {gm},
-  timestamp = {2007.08.06}
+  volume = {26},  number = {3},
+  pages = {320--340}
 }
 
@@ -3365 +2294 @@
   title = {The role of internal tides in mixing the deep ocean},
   journal = JPO,
-  pages = {2882--2899},
-  owner = {gm},
-  timestamp = {2010.05.20}
+  pages = {2882--2899}
 }
 
 @ARTICLE{St_Laurent_Nash_DSR04,
   author = {L.C. {St. Laurent} and J. D. Nash},
-  title = {An examination of the radiative and dissipative properties of deep
-   ocean internal tides},
+  title = {An examination of the radiative and dissipative properties of deep ocean internal tides},
   journal = DSR,
   year = {2004},
-  volume = {II, 51},
+  volume = {II},  number = {51},
   pages = {3029--3042},
   doi = {10.1016/j.dsr2.2004.09.008},
-  owner = {gm},
-  timestamp = {2010.05.21},
   url = {http://dx.doi.org/10.1016/j.dsr2.2004.09.008}
 }
@@ -3392 +2316 @@
   pages = {2106},
   doi = {10.1029/2002GL015633},
-  owner = {gm},
-  timestamp = {2010.05.20},
   url = {http://dx.doi.org/10.1029/2002GL015633}
 }
@@ -3402 +2324 @@
   journal = JC,
   year = {2001},
-  volume = {14},
-  pages = {2079--2087
-   
-   },
-  number = {9},
-  abstract = {A new gridded ocean climatology, the Polar Science Center Hydrographic
-   Climatology (PHC), has been created that merges the 1998 version
-   of the World Ocean Atlas with the new regional Arctic Ocean Atlas.
-   The result is a global climatology for temperature and salinity that
-   contains a good description of the Arctic Ocean and its environs.
-   Monthly, seasonal, and annual average products have been generated.
-   How the original datasets were prepared for merging, how the optimal
-   interpolation procedure was performed, and characteristics of the
-   resulting dataset are discussed, followed by a summary and discussion
-   of future plans.},
-  date = {May 01, 2001},
-  owner = {gm},
-  timestamp = {2007.08.06}
+  volume = {14},  number = {9},
+  pages = {2079--2087},
 }
 
 @ARTICLE{Stein_Stein_Nat92,
   author = {C. A. Stein and S. Stein},
-  title = {A model for the global variation in oceanic depth and heat flow with
-   lithospheric age},
+  title = {A model for the global variation in oceanic depth and heat flow with lithospheric age},
   journal = {Nature},
   year = {1992},
   volume = {359},
-  pages = {123--129},
-  owner = {gm},
-  timestamp = {2007.08.04}
+  pages = {123--129}
 }
 
 @ARTICLE{Thiem_Berntsen_OM06,
   author = {O. Thiem and J. Berntsen},
-  title = {Internal pressure errors in sigma-coordinate ocean models due to
-   anisotropy},
+  title = {Internal pressure errors in sigma-coordinate ocean models due to anisotropy},
   journal = OM,
   year = {2006},
-  volume = {12, 1-2},
-  owner = {gm},
-  timestamp = {2007.08.05}
+  volume = {12},  number = {1-2},
 }
 
 @ARTICLE{Timmermann_al_OM05,
-  author = {R. Timmermann and H. Goosse and G. Madec and T. Fichefet, and C.
-   Ethe and V. Duli\`{e}re},
-  title = {On the representation of high latitude processes in the ORCA-LIM
-   global coupled 
-   
-   sea ice-ocean model.},
+  author = {R. Timmermann and H. Goosse and G. Madec and T. Fichefet, and C. \'{E}the and V. Duli\`{e}re},
+  title = {On the representation of high latitude processes in the ORCA-LIM global coupled sea ice-ocean model},
   journal = OM,
   year = {2005},
   volume = {8},
-  pages = {175–201},
-  owner = {gm},
-  timestamp = {2008.07.05}
+  pages = {175--201}
 }
 
 @ARTICLE{Treguier_JGR92,
   author = {A.M. Tr\'{e}guier},
-  title = {Kinetic energy analysis of an eddy resolving, primitive equation
-   North Atlantic model},
+  title = {Kinetic energy analysis of an eddy resolving, primitive equation North Atlantic model},
   journal = JGR,
   year = {1992},
   volume = {97},
-  pages = {687-701}
+  pages = {687--701}
 }
 
 @ARTICLE{Treguier_al_JGR01,
-  author = {A.M Tr\'{e}guier and B. Barnier and A.P. de Miranda and J.M. Molines
-   and N. Grima and M. Imbard and G. Madec and C. Messager and T. Reynaud
-   and S. Michel},
-  title = {An Eddy Permitting model of the Atlantic circulation: evaluating
-   open boundary conditions},
+  author = {A.M. Tr\'{e}guier and B. Barnier and A.P. de Miranda and J.M. Molines
+    and N. Grima and M. Imbard and G. Madec and C. Messager and T. Reynaud and S. Michel},
+  title = {An Eddy Permitting model of the Atlantic circulation: evaluating open boundary conditions},
   journal = JGR,
   year = {2001},
@@ -3487 +2378 @@
   journal = DSR,
   year = {2003},
-  pages = {251--280},
-  owner = {gm},
-  timestamp = {2009.08.20}
+  pages = {251--280}
 }
 
 @ARTICLE{Treguier1996,
   author = {A.-M. Tr\'{e}guier and J. Dukowicz and K. Bryan},
-  title = {Properties of nonuniform grids used in ocean general circulation
-   models},
+  title = {Properties of nonuniform grids used in ocean general circulation models},
   journal = JGR,
   year = {1996},
   volume = {101},
-  pages = {20,877--20,881},
-  owner = {gm},
-  timestamp = {2007.08.03}
+  pages = {20,877--20,881}
 }
 
 @ARTICLE{Treguier_al_OS07,
-  author = {A.-M. Tr\'{e}guier and M. H. England and S. R. Rintoul and G. Madec
-   and J. Le Sommer and J.-M. Molines},
-  title = {Southern Ocean overturning across streamlines in an eddying simulation
-   of the Antarctic Circumpolar Current},
+  author = {A.-M. Tr\'{e}guier and M. H. England and S. R. Rintoul and G. Madec and J. Le Sommer and J.-M. Molines},
+  title = {Southern Ocean overturning across streamlines in an eddying simulation of the Antarctic Circumpolar Current},
   journal = OS,
   year = {2007},
   volume = {4},
-  pages = {653--698},
-  owner = {gm},
-  timestamp = {2009.08.19}
+  pages = {653--698}
 }
 
 @ARTICLE{Treguier_al_OD06,
-  author = {A.-M. Tr\'{e}guier and C. Gourcuff and P. Lherminier and H. Mercier
-   and B. Barnier and G. Madec and J.-M. Molines and T. Penduff and
-   L. Czeschel and C. Böning},
+  author = {A.-M. Tr\'{e}guier and C. Gourcuff and P. Lherminier and H. Mercier and B. Barnier 
+  and G. Madec and J.-M. Molines and T. Penduff and L. Czeschel and C. Böning},
   title = {Internal and forced variability along a section between Greenland
    and Portugal in the CLIPPER Atlantic model},
@@ -3528 +2409 @@
   pages = {568--580},
   doi = {10.1007/s10236-006-0069-y},
-  owner = {gm},
-  timestamp = {2009.08.19},
   url = {http://dx.doi.org/10.1007/s10236-006-0069-y}
 }
@@ -3535 +2414 @@
 @ARTICLE{Treguier1997,
   author = {A. M. Tr\'{e}guier and I. M. Held and V. D. Larichev},
-  title = {Parameterization of Quasigeostrophic Eddies in Primitive Equation
-   Ocean Models},
+  title = {Parameterization of Quasigeostrophic Eddies in Primitive Equation Ocean Models},
   journal = JPO,
   year = {1997},
-  volume = {27},
-  pages = {567--580},
-  number = {4},
-  abstract = {A parameterization of mesoscale eddy fluxes in the ocean should be
-   consistent with the fact that the ocean interior is nearly adiabatic.
-   Gent and McWilliams have described a framework in which this can
-   be approximated in z-coordinate primitive equation models by incorporating
-   the effects of eddies on the buoyancy field through an eddy-induced
-   velocity. It is also natural to base a parameterization on the simple
-   picture of the mixing of potential vorticity in the interior and
-   the mixing of buoyancy at the surface. The authors discuss the various
-   constraints imposed by these two requirements and attempt to clarify
-   the appropriate boundary conditions on the eddy-induced velocities
-   at the surface. Quasigeostrophic theory is used as a guide to the
-   simplest way of satisfying these constraints.},
-  date = {April 01, 1997},
-  owner = {gm},
-  timestamp = {2007.08.03}
+  volume = {27},  number = {4},
+  pages = {567--580}
 }
 
@@ -3564 +2426 @@
   journal = {JMS}, 
   year = {2003},
-  volume = {61},
-  pages = {235--265},
-  number = {2},
-  owner = {gr},
-  timestamp = {2010.09.09}
+  volume = {61},  number = {2},
+  pages = {235--265}
 }
 
@@ -3577 +2436 @@
   year = {2005},
   volume = {25},
-  pages = {795--827},
-  owner = {gm},
-  timestamp = {2010.09.09}
+  pages = {795--827}
 }
 
@@ -3586 +2443 @@
   publisher = {Techn. Paper in Mar. Sci, 44, UNESCO},
   year = {1983},
-  author = {UNESCO},
-  owner = {gm},
-  timestamp = {2007.08.04}
+  author = {UNESCO}
 }
 
@@ -3594 +2449 @@
   author = {S. Valcke},
   title = {OASIS3 User Guide (prism\_2-5)},
-  institution = {PRISM Support Initiative Report No 3, CERFACS, Toulouse, France,
-   64 pp},
+  institution = {PRISM Support Initiative Report No 3, CERFACS, Toulouse, France},
   year = {2006},
-  owner = {gm},
-  timestamp = {2007.08.05}
+  pages = {64pp}
 }
 
@@ -3606 +2459 @@
   institution = {CERFACS},
   year = {2000},
-  number = {TR/CMGC/00-10},
-  owner = {gm}
+  number = {TR/CMGC/00-10}
 }
 
 @ARTICLE{Vancoppenolle_al_OM09b,
   author = {M. Vancoppenolle and T. Fichefet and H. Goosse},
-  title = {Simulating the mass balance and salinity of Arctic and Antarctic
-   sea ice. 2. Importance of sea ice salinity variations},
+  title = {Simulating the mass balance and salinity of Arctic and Antarctic sea ice. 2. 
+     Importance of sea ice salinity variations},
   journal = {0M},
   year = {2009},
   volume = {27},
-  pages = {54--69},
-  owner = {gm},
-  timestamp = {2009.08.20}
+  pages = {54--69}
 }
 
@@ -3632 +2482 @@
   pages = {33--53},
   doi = {10.1016/j.ocemod.2008.10.005},
-  owner = {gm},
-  timestamp = {2008.07.05},
   url = {http://dx.doi.org/10.1016/j.ocemod.2008.10.005}
 }
@@ -3644 +2492 @@
   journal = JPO,
   year = {2001},
-  volume = {31, 7},
-  pages = {1649--1675},
-  owner = {gm},
-  timestamp = {2009.08.20}
+  volume = {31},  number = {7},
+  pages = {1649--1675}
 }
 
@@ -3655 +2501 @@
   journal = JMR,
   year = {1984},
-  volume = {42, 2},
-  pages = {289-301},
-  owner = {gm},
-  timestamp = {2007.08.06}
+  volume = {42},  number = {2},
+  pages = {289-301}
 }
 
@@ -3664 +2508 @@
   author = {A. J. Weaver and M. Eby},
   title = {On the numerical implementation of advection schemes for use in conjuction
-   with various mixing 
-   
-   parameterizations in the GFDL ocean model},
+   with various mixing parameterizations in the GFDL ocean model},
   journal = JPO,
   year = {1997},
-  volume = {27},
-  owner = {gm},
-  timestamp = {2007.08.06}
+  volume = {27}
 }
 
@@ -3679 +2519 @@
   journal = JAOT,
   year = {1998},
-  volume = {15},
+  volume = {15},  number = {5},
   pages = {1171-1187},
-  number = {5},
-  abstract = {Leonard’s widely used QUICK advection scheme is, like the Bryan–Cox–Semtner
-   ocean model, based on a control volume form of the advection equation.
-   Unfortunately, in its normal form it cannot be used with the leapfrog–Euler
-   forward time-stepping schemes used by the ocean model. Farrow and
-   Stevens overcame the problem by implementing a predictor–corrector
-   time-stepping scheme, but this is computationally expensive to run.
-   The present paper shows that the problem can be overcome by splitting
-   the QUICK operator into an O(δx2) advective term and a velocity
-   dependent biharmonic diffusion term. These can then be time-stepped
-   using the combined leapfrog and Euler forward schemes of the Bryan–Cox–Semtner
-   ocean model, leading to a significant increase in model efficiency.
-   A small change in the advection operator coefficients may also be
-   made leading to O(δx4) accuracy. Tests of the improved schemes
-   are carried out making use of a global eddy-permitting ocean model.
-   Results are presented from cases where the schemes were applied to
-   only the tracer fields and also from cases where they were applied
-   to both the tracer and velocity fields. It is found that the new
-   schemes have the most effect in the western boundary current regions,
-   where, for example, the warm core of the Agulhas Current is no longer
-   broken up by numerical noise.},
-  date = {October 01, 1998},
-  owner = {gm},
-  timestamp = {2007.08.04}
 }
 
@@ -3714 +2530 @@
   year = {2009},
   volume = {228},
-  pages = {8665--8692},
-  owner = {gm},
-  timestamp = {2010.04.14}
+  pages = {8665--8692}
 }
 
@@ -3724 +2538 @@
   journal = {AIAA journal},
   year = {1988},
-  volume = {26, 11},
-  pages = {1299--1310},
-  owner = {gr},
-  timestamp = {2010.09.09}
+  volume = {26},  number = {11},
+  pages = {1299--1310}
 }
 
 @ARTICLE{Willebrand_al_PO01,
   author = {J. Willebrand and B. Barnier and C. Boning and C. Dieterich and P.
-   D. Killworth and C. Le Provost and Y. Jia and J.-M. Molines and A.
-   L. New},
-  title = {Circulation characteristics in three eddy-permitting models of the
-   North Atlantic},
+   D. Killworth and C. Le Provost and Y. Jia and J.-M. Molines and A. L. New},
+  title = {Circulation characteristics in three eddy-permitting models of the North Atlantic},
   journal = PO,
   year = {2001},
-  volume = {48, 2},
-  pages = {123--161},
-  owner = {gm},
-  timestamp = {2007.08.04}
+  volume = {48},  number = {2},
+  pages = {123--161}
 }
 
 @ARTICLE{Williams_al_DAO09,
-  author = {P.D. Williams and E. Guilyardi and G. Madec and S. Gualdi and E.
-   Scoccimarro},
+  author = {P.D. Williams and E. Guilyardi and G. Madec and S. Gualdi and E. Scoccimarro},
   title = {The role of mean ocean salinity on climate},
   journal = DAO,
-  year = {2009},
-  volume = {in press},
-  owner = {gm},
-  timestamp = {2009.08.19}
+  year = {2010},
+  volume = {49},  number = {2-3},
+  pages = {108--123},
+  doi = {10.1016/j.dynatmoce.2009.02.001},
+  url = {http://dx.doi.org/10.1016/j.dynatmoce.2009.02.001}
 }
 
 @ARTICLE{Williams_al_GRL07,
-  author = {P.D. Williams and E. Guilyardi and R. Sutton and J.M. Gregory and
-   G. Madec},
+  author = {P.D. Williams and E. Guilyardi and R. Sutton and J.M. Gregory and G. Madec},
   title = {A new feedback on climate change from the hydrological cycle},
   journal = GRL,
@@ -3764 +2571 @@
   pages = {L08706},
   doi = {10.1029/2007GL029275},
-  owner = {gm},
-  timestamp = {2009.08.19},
   url = {http://dx.doi.org/10.1029/2007GL029275}
 }
 
 @ARTICLE{Williams_al_CD06,
-  author = {P.D. Williams and E. Guilyardi and R. Sutton and J.M. Gregory and
-   G. Madec},
-  title = {On the climate response of the low-latitude Pacific ocean to changes
-   in the global freshwater cycle},
+  author = {P.D. Williams and E. Guilyardi and R. Sutton and J.M. Gregory and G. Madec},
+  title = {On the climate response of the low-latitude Pacific ocean to changes in the global freshwater cycle},
   journal = CD,
   year = {2006},
   volume = {27},
-  pages = {593--611},
-  owner = {gm},
-  timestamp = {2009.08.19}
+  pages = {593--611}
 }
 
@@ -3787 +2588 @@
   journal = JCP,
   year = {1979},
-  volume = {31},
-  owner = {gm},
-  timestamp = {2007.08.04}
+  volume = {31}
 }
 
 @ARTICLE{Zhang_Endoh_JGR92,
   author = {Zhang, R.-H. and Endoh, M.},
-  title = {A free surface general circulation model for the tropical Pacific
-   Ocean},
+  title = {A free surface general circulation model for the tropical Pacific Ocean},
   journal = JGR,
   year = {1992},
   volume = {97},
-  pages = {11,237--11,255},
-  month = jul,
-  owner = {gm}
+  pages = {11,237--11,255}
 }