Changeset 11123 for NEMO/trunk/doc/latex/NEMO/subfiles/chap_DIA.tex

Timestamp:

2019-06-17T14:22:27+02:00 (5 years ago)

Author:

nicolasmartin

Message:

Modification of LaTeX subfiles accordingly to new citations keys

Location:

NEMO/trunk/doc/latex/NEMO/subfiles

Files:

• . (modified) (1 prop)
• chap_DIA.tex (modified) (6 diffs)

NEMO/trunk/doc/latex/NEMO/subfiles/chap_DIA.tex

@@ -1507 +1507 @@
 remain at a given depth ($w = 0$ in the computation) have been introduced in the system during the CLIPPER project.
 Options are defined by \ngn{namflo} namelis variables.
-The algorithm used is based either on the work of \cite{Blanke_Raynaud_JPO97} (default option),
+The algorithm used is based either on the work of \cite{blanke.raynaud_JPO97} (default option),
 or on a $4^th$ Runge-Hutta algorithm (\np{ln\_flork4}\forcode{ = .true.}).
-Note that the \cite{Blanke_Raynaud_JPO97} algorithm have the advantage of providing trajectories which
+Note that the \cite{blanke.raynaud_JPO97} algorithm have the advantage of providing trajectories which
 are consistent with the numeric of the code, so that the trajectories never intercept the bathymetry.
 
@@ -1809 +1809 @@
 The steric effect is therefore not explicitely represented.
 This approximation does not represent a serious error with respect to the flow field calculated by the model
-\citep{Greatbatch_JGR94}, but extra attention is required when investigating sea level,
+\citep{greatbatch_JGR94}, but extra attention is required when investigating sea level,
 as steric changes are an important contribution to local changes in sea level on seasonal and climatic time scales.
 This is especially true for investigation into sea level rise due to global warming.
 
 Fortunately, the steric contribution to the sea level consists of a spatially uniform component that
-can be diagnosed by considering the mass budget of the world ocean \citep{Greatbatch_JGR94}.
+can be diagnosed by considering the mass budget of the world ocean \citep{greatbatch_JGR94}.
 In order to better understand how global mean sea level evolves and thus how the steric sea level can be diagnosed,
 we compare, in the following, the non-Boussinesq and Boussinesq cases.
@@ -1888 +1888 @@
 the ocean surface, not by changes in mean mass of the ocean: the steric effect is missing in a Boussinesq fluid.
 
-Nevertheless, following \citep{Greatbatch_JGR94}, the steric effect on the volume can be diagnosed by
+Nevertheless, following \citep{greatbatch_JGR94}, the steric effect on the volume can be diagnosed by
 considering the mass budget of the ocean. 
 The apparent changes in $\mathcal{M}$, mass of the ocean, which are not induced by surface mass flux
 must be compensated by a spatially uniform change in the mean sea level due to expansion/contraction of the ocean
-\citep{Greatbatch_JGR94}.
+\citep{greatbatch_JGR94}.
 In others words, the Boussinesq mass, $\mathcal{M}_o$, can be related to $\mathcal{M}$,
 the total mass of the ocean seen by the Boussinesq model, via the steric contribution to the sea level,
@@ -1924 +1924 @@
 This value is a sensible choice for the reference density used in a Boussinesq ocean climate model since,
 with the exception of only a small percentage of the ocean, density in the World Ocean varies by no more than
-2$\%$ from this value (\cite{Gill1982}, page 47).
+2$\%$ from this value (\cite{gill_bk82}, page 47).
 
 Second, we have assumed here that the total ocean surface, $\mathcal{A}$,
@@ -1954 +1954 @@
 so that there are no associated ocean currents.
 Hence, the dynamically relevant sea level is the effective sea level,
-\ie the sea level as if sea ice (and snow) were converted to liquid seawater \citep{Campin_al_OM08}.
+\ie the sea level as if sea ice (and snow) were converted to liquid seawater \citep{campin.marshall.ea_OM08}.
 However, in the current version of \NEMO the sea-ice is levitating above the ocean without mass exchanges between
 ice and ocean.
@@ -1986 +1986 @@
 Among the available diagnostics the following ones are obtained when defining the \key{diahth} CPP key:
 
-- the mixed layer depth (based on a density criterion \citep{de_Boyer_Montegut_al_JGR04}) (\mdl{diahth})
+- the mixed layer depth (based on a density criterion \citep{de-boyer-montegut.madec.ea_JGR04}) (\mdl{diahth})
 
 - the turbocline depth (based on a turbulent mixing coefficient criterion) (\mdl{diahth})