Index: trunk/DOC/TexFiles/Bibliography/Biblio.bib
===================================================================
--- trunk/DOC/TexFiles/Bibliography/Biblio.bib	(revision 6997)
+++ trunk/DOC/TexFiles/Bibliography/Biblio.bib	(revision 7646)
@@ -472,4 +472,16 @@
 }
 
+@article{bouffard_Boegman_DAO2013,
+	author = {D. Bouffard and L. Boegman},
+	title = {A diapycnal diffusivity model for stratified environmental flows},
+	volume = {61-62},
+	issn = {03770265},
+	url = {http://dx.doi.org/10.1016/j.dynatmoce.2013.02.002},
+	doi = {10.1016/j.dynatmoce.2013.02.002},
+	journal = DAO,
+	year = {2013},
+	pages = {14--34},
+}
+
 @ARTICLE{Bougeault1989,
   author = {P. Bougeault and P. Lacarrere},
@@ -787,4 +799,28 @@
   volume = {34},
   pages = {8--13}
+}
+
+@article{de_lavergne_JPO2016_mixing,
+	author = {C. de Lavergne and G. Madec and J. Le Sommer and A. J. G. Nurser and A. C. Naveira Garabato },
+	title = {On Antarctic Bottom Water consumption in the abyssal ocean},
+	issn = {0022-3670},
+	url = {http://dx.doi.org/10.1175/JPO-D-14-0201.1},
+	doi = {10.1175/JPO-D-14-0201.1},
+	abstract = {In studies of ocean mixing, it is generally assumed that small-scale turbulent overturns lose 15-20 \% of their energy in eroding the background stratification. Accumulating evidence that this energy fraction, or mixing efficiency Rf, significantly varies depending on flow properties challenges this assumption, however. Here, we examine the implications of a varying mixing efficiency for ocean energetics and deep water mass transformation. Combining current parameterizations of internal wave-driven mixing with a recent model expressing Rf as a function of a turbulence intensity parameter Reb = εν/νN2, we show that accounting for reduced mixing efficiencies in regions of weak stratification or energetic turbulence (high Reb) strongly limits the ability of breaking internal waves to supply oceanic potential energy and drive abyssal upwelling. Moving from a fixed Rf = 1/6 to a variable efficiency Rf(Reb) causes Antarctic Bottom Water upwelling induced by locally-dissipating internal tides and lee waves to fall from 9 to 4 Sv, and the corresponding potential energy source to plunge from 97 to 44 GW. When adding the contribution of remotely-dissipating internal tides under idealized distributions of energy dissipation, the total rate of Antarctic Bottom Water upwelling is reduced by about a factor of 2, reaching 5-15 Sv compared to 10-33 Sv for a fixed efficiency. Our results suggest that distributed mixing, overflow-related boundary processes and geothermal heating are more effective in consuming abyssal waters than topographically-enhanced mixing by breaking internal waves. Our calculations also point to the importance of accurately constraining Rf(Reb) and including the effect in ocean models.},
+	journal = {Journal of Physical Oceanography},
+	year = {2016},
+	volume = {46},  pages = {635-–661}
+}
+
+@article{de_lavergne_JPO2016_efficiency,
+	author = {C. de Lavergne and G. Madec and J. Le Sommer and A. J. G. Nurser and A. C. Naveira Garabato },
+	title = {The impact of a variable mixing efficiency on the abyssal overturning},
+	issn = {0022-3670},
+	url = {http://dx.doi.org//10.1175/JPO-D-14-0259.1},
+	doi = {10.1175/JPO-D-14-0259.1},
+	abstract = {In studies of ocean mixing, it is generally assumed that small-scale turbulent overturns lose 15-20 \% of their energy in eroding the background stratification. Accumulating evidence that this energy fraction, or mixing efficiency Rf, significantly varies depending on flow properties challenges this assumption, however. Here, we examine the implications of a varying mixing efficiency for ocean energetics and deep water mass transformation. Combining current parameterizations of internal wave-driven mixing with a recent model expressing Rf as a function of a turbulence intensity parameter Reb = εν/νN2, we show that accounting for reduced mixing efficiencies in regions of weak stratification or energetic turbulence (high Reb) strongly limits the ability of breaking internal waves to supply oceanic potential energy and drive abyssal upwelling. Moving from a fixed Rf = 1/6 to a variable efficiency Rf(Reb) causes Antarctic Bottom Water upwelling induced by locally-dissipating internal tides and lee waves to fall from 9 to 4 Sv, and the corresponding potential energy source to plunge from 97 to 44 GW. When adding the contribution of remotely-dissipating internal tides under idealized distributions of energy dissipation, the total rate of Antarctic Bottom Water upwelling is reduced by about a factor of 2, reaching 5-15 Sv compared to 10-33 Sv for a fixed efficiency. Our results suggest that distributed mixing, overflow-related boundary processes and geothermal heating are more effective in consuming abyssal waters than topographically-enhanced mixing by breaking internal waves. Our calculations also point to the importance of accurately constraining Rf(Reb) and including the effect in ocean models.},
+	journal = {Journal of Physical Oceanography},
+	year = {2016},
+	volume = {46},  pages = {663-–681}
 }
 
@@ -1160,4 +1196,18 @@
 }
 
+@article{goff_JGR2010,
+	author = {J. A. Goff},
+	title = {Global prediction of abyssal hill root-mean-square heights from small-scale altimetric gravity variability},
+	issn = {2156-2202},
+	url = {http://dx.doi.org/10.1029/2010JB007867},
+	doi = {10.1029/2010JB007867},
+	abstract = {Abyssal hills, which are pervasive landforms on the seafloor of the Earth's oceans, represent a potential tectonic record of the history of mid-ocean ridge spreading. However, the most detailed global maps of the seafloor, derived from the satellite altimetry-based gravity field, cannot be used to deterministically characterize such small-scale ({\textless}10 km) morphology. Nevertheless, the small-scale variability of the gravity field can be related to the statistical properties of abyssal hill morphology using the upward continuation formulation. In this paper, I construct a global prediction of abyssal hill root-mean-square (rms) heights from the small-scale variability of the altimetric gravity field. The abyssal hill-related component of the gravity field is derived by first masking distinct features, such as seamounts, mid-ocean ridges, and continental margins, and then applying a newly designed adaptive directional filter algorithm to remove fracture zone/discontinuity fabric. A noise field is derived empirically by correlating the rms variability of the small-scale gravity field to the altimetric noise field in regions of very low relief, and the noise variance is subtracted from the small-scale gravity variance. Suites of synthetically derived, abyssal hill formed gravity fields are generated as a function of water depth, basement rms heights, and sediment thickness and used to predict abyssal hill seafloor rms heights from corrected small-scale gravity rms height. The resulting global prediction of abyssal hill rms heights is validated qualitatively by comparing against expected variations in abyssal hill morphology and quantitatively by comparing against actual measurements of rms heights. Although there is scatter, the prediction appears unbiased.},
+	volume = {115},
+	number = {B12},
+	journal = {Journal of Geophysical Research: Solid Earth},
+	year = {2010},
+	pages = {B12104},
+}
+
 @ARTICLE{Goosse_al_JGR99,
   author = {H. Goosse and E. Deleersnijder and T. Fichefet and M. England},
@@ -1264,6 +1314,6 @@
 
 @ARTICLE{Griffies_Hallberg_MWR00,
-  author = {S.M. Griffies and R.H. Hallberg},
-  title = {Biharmonic friction with a smagorinsky-like viscosity for use in large-scale eddy-permitting ocean models},
+  author = {S.M. Griffies and R.W. Hallberg},
+  title = {Biharmonic friction with a Smagorinsky-like viscosity for use in large-scale eddy-permitting ocean models},
   journal = MWR,
   year = {2000},
@@ -1586,4 +1636,17 @@
   volume = {12},
   pages = {381--389}
+}
+
+@article{Jackson_Rehmann_JPO2014,
+	author = {P. R. Jackson and C. R. Rehmann},
+	title = {Experiments on differential scalar mixing in turbulence in a sheared, stratified flow},
+	journal = JPO,
+	volume = {44},
+	issn = {0022-3670},
+	url = {http://dx.doi.org/10.1175/JPO-D-14-0027.1},
+	doi = {10.1175/JPO-D-14-0027.1},
+	number = {10},
+	year = {2014},
+	pages = {2661--2680},
 }
 
@@ -1936,5 +1999,5 @@
   year = {2009},
   volume = {30},  number = {2-3},
-  pages = {88--94},
+  pages = {88-94},
   doi = {10.1016/j.ocemod.2009.06.006},
   url = {http://dx.doi.org/10.1016/j.ocemod.2009.06.006}
@@ -2430,4 +2493,14 @@
 }
 
+@ARTICLE{Morel_Berthon_LO89,
+  author = {A. Morel and J.-F. Berthon},
+  title = {Surface pigments, algal biomass profiles, and potential production of the euphotic layer: 
+           Relationships reinvestigated in view of remote-sensing applications},
+  journal = {Limnol. Oceanogr.},
+  year = {1989},
+  volume = {34(8)},
+  pages = {1545--1562}
+}
+
 @ARTICLE{Morel_Maritorena_JGR01,
   author = {A. Morel and S. Maritorena},
@@ -2476,6 +2549,7 @@
 @ARTICLE{Osborn_JPO80,
   author = {T.R. Osborn},
-  title = {Estimates of the local rate of vertical diﬀusion from dissipation measurements},
-  journal = JPO,
+  title = {Estimates of the local rate of vertical diffusion from dissipation measurements},
+  journal = JPO,
+  year = {1980},
   volume = {10},
   pages = {83--89}
@@ -2714,4 +2788,15 @@
 }
 
+@ARTICLE{Rousset_GMD2015,
+  author = {C. Rousset and M. Vancoppenolle and G. Madec and T. Fichefet and S. Flavoni 
+            and A. Barth\'{e}lemy and R. Benshila and J. Chanut and C. L\'{e}vy and S. Masson and F. Vivier },
+  title  = {The Louvain-La-Neuve sea-ice model LIM3.6: Global and regional capabilities},
+  journal= {Geoscientific Model Development},
+  year = {2015},
+  volume = {8}, pages={2991--3005},
+  doi = {10.5194/gmd-8-2991-2015},
+  url = {http://dx.doi.org/10.5194/gmd-8-2991-2015}
+}
+
 @ARTICLE{Sadourny1975,
   author = {R. Sadourny},
@@ -2794,4 +2879,13 @@
   year = {2004},
   pages = {245--263},
+}
+
+@INBOOK{Smagorinsky_93,
+  author = {Smagorinsky, J.},
+  chapter = {Some historical remarks on the use of non-linear viscosities},
+  title = {Large Eddy Simulation of Complex Engineering and Geophysical Flows},
+  pages = {3--36},
+  year = {1993},
+  publisher = {Cambridge University Press, B. Galperin and S. A. Orszag (eds.)},
 }
 
