Changeset 10468 for NEMO/trunk/doc/latex/NEMO/subfiles/chap_DYN.tex

Timestamp:

2019-01-08T12:34:39+01:00 (5 years ago)

Author:

mathiot

Message:

update ISF documentation (DYN and SBC)

File:

• NEMO/trunk/doc/latex/NEMO/subfiles/chap_DYN.tex (modified) (2 diffs)

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

@@ -697 +697 @@
 \label{subsec:DYN_hpg_isf}
 Beneath an ice shelf, the total pressure gradient is the sum of the pressure gradient due to the ice shelf load and
-the pressure gradient due to the ocean load.
-If cavity opened (\np{ln\_isfcav}\forcode{ = .true.}) these 2 terms can be calculated by
-setting \np{ln\_dynhpg\_isf}\forcode{ = .true.}.
-No other scheme are working with the ice shelf.\\
-
-$\bullet$ The main hypothesis to compute the ice shelf load is that the ice shelf is in an isostatic equilibrium.
+the pressure gradient due to the ocean load (\np{ln\_dynhpg\_isf}\forcode{ = .true.}).\\
+
+The main hypothesis to compute the ice shelf load is that the ice shelf is in an isostatic equilibrium.
 The top pressure is computed integrating from surface to the base of the ice shelf a reference density profile
 (prescribed as density of a water at 34.4 PSU and -1.9\deg{C}) and
@@ -709 +706 @@
 A detailed description of this method is described in \citet{Losch2008}.\\
 
-$\bullet$ The ocean load is computed using the expression \autoref{eq:dynhpg_sco} described in
+The pressure gradient due to ocean load is computed using the expression \autoref{eq:dynhpg_sco} described in
 \autoref{subsec:DYN_hpg_sco}.