Changeset 2205 for branches/DEV_r2191_3partymerge2010/DOC/TexFiles/Chapters/Chap_Model_Basics_zstar.tex

Timestamp:

2010-10-11T18:24:37+02:00 (14 years ago)

Author:

acc

Message:

#733 DEV_r2191_3partymerge2010. Merged in changes from DEV_r1924_nocs_latphys

File:

• branches/DEV_r2191_3partymerge2010/DOC/TexFiles/Chapters/Chap_Model_Basics_zstar.tex (modified) (1 diff)

branches/DEV_r2191_3partymerge2010/DOC/TexFiles/Chapters/Chap_Model_Basics_zstar.tex

@@ -119 +119 @@
 \begin{figure}[!t] \label{Fig_DYN_dynspg_ts}
 \begin{center}
-\includegraphics[width=0.90\textwidth]{./Figures/Fig_DYN_dynspg_ts.pdf}
+\includegraphics[width=0.90\textwidth]{./TexFiles/Figures/Fig_DYN_dynspg_ts.pdf}
 \caption{Schematic of the split-explicit time stepping scheme for the barotropic and baroclinic modes, after \citet{Griffies2004}. Time increases to the right. Baroclinic time steps are denoted by $t-\Delta t$, $t, t+\Delta t$, and $t+2\Delta t$. The curved line represents a leap-frog time step, and the smaller barotropic time steps $N \Delta t=2\Delta t$ are denoted by the zig-zag line. The vertically integrated forcing \textbf{M}(t) computed at baroclinic time step t represents the interaction between the barotropic and baroclinic motions. While keeping the total depth, tracer, and freshwater forcing fields fixed, a leap-frog integration carries the surface height and vertically integrated velocity from t to $t+2 \Delta t$ using N barotropic time steps of length $\Delta t$. Time averaging the barotropic fields over the N+1 time steps (endpoints included) centers the vertically integrated velocity at the baroclinic timestep $t+\Delta t$. A baroclinic leap-frog time step carries the surface height to $t+\Delta t$ using the convergence of the time averaged vertically integrated velocity taken from baroclinic time step t. }
 \end{center}