11 |
\subsubsection{Introduction |
\subsubsection{Introduction |
12 |
\label{sec:pkg:obcs:intro}} |
\label{sec:pkg:obcs:intro}} |
13 |
|
|
14 |
|
The OBCS-package is fundamental to regional ocean modelling with the |
15 |
|
MITgcm, but there are so many details to be considered in |
16 |
|
regional ocean modelling that this package cannot accomodate all |
17 |
|
imaginable and possible options. Therefore, for a regional simulation |
18 |
|
with very particular details, it is recommended to familiarize oneself |
19 |
|
not only with the compile- and runtime-options of this package, but |
20 |
|
also with the code itself. In many cases it will be necessary to adapt |
21 |
|
the obcs-code (in particular \code{S/R OBCS\_CALC}) to the application |
22 |
|
in question; in these cases the obcs-package (together with the |
23 |
|
rbcs-package, section \ref{sec:pkg:rbcs}) is a very |
24 |
|
useful infrastructure for implementing special regional models. |
25 |
|
|
26 |
%---------------------------------------------------------------------- |
%---------------------------------------------------------------------- |
27 |
|
|
34 |
\begin{itemize} |
\begin{itemize} |
35 |
% |
% |
36 |
\item |
\item |
37 |
using the \texttt{packages.conf} file by adding \texttt{obcs} to it, |
using the \code{packages.conf} file by adding \code{obcs} to it, |
38 |
% |
% |
39 |
\item |
\item |
40 |
or using \texttt{genmake2} adding |
or using \code{genmake2} adding |
41 |
\texttt{-enable=obcs} or \texttt{-disable=obcs} switches |
\code{-enable=obcs} or \code{-disable=obcs} switches |
42 |
% |
% |
43 |
\item |
\item |
44 |
\textit{Required packages and CPP options:} \\ |
\textit{Required packages and CPP options:} \\ |
47 |
which differ in the way how OB's are treated in time: |
which differ in the way how OB's are treated in time: |
48 |
A simple time-management (e.g. constant in time, or cyclic with |
A simple time-management (e.g. constant in time, or cyclic with |
49 |
fixed fequency) is provided through |
fixed fequency) is provided through |
50 |
S/R \texttt{obcs\_external\_fields\_load}. |
S/R \code{obcs\_external\_fields\_load}. |
51 |
More sophisticated ``real-time'' (i.e. calendar time) management is |
More sophisticated ``real-time'' (i.e. calendar time) management is |
52 |
available through \texttt{obcs\_prescribe\_read}. |
available through \code{obcs\_prescribe\_read}. |
53 |
The latter case requires |
The latter case requires |
54 |
packages \texttt{cal} and \texttt{exf} to be enabled. |
packages \code{cal} and \code{exf} to be enabled. |
55 |
% |
% |
56 |
\end{itemize} |
\end{itemize} |
57 |
(see also Section \ref{sec:buildingCode}). |
(see also Section \ref{sec:buildingCode}). |
58 |
|
|
59 |
Parts of the OBCS code can be enabled or disabled at compile time |
Parts of the OBCS code can be enabled or disabled at compile time |
60 |
via CPP preprocessor flags. These options are set in |
via CPP preprocessor flags. These options are set in |
61 |
\texttt{OBCS\_OPTIONS.h}. Table \ref{tab:pkg:obcs:cpp} summarizes them. |
\code{OBCS\_OPTIONS.h}. Table \ref{tab:pkg:obcs:cpp} summarizes them. |
62 |
|
|
63 |
\begin{table}[!ht] |
\begin{table}[!ht] |
64 |
\centering |
\centering |
68 |
\hline |
\hline |
69 |
\textbf{CPP option} & \textbf{Description} \\ |
\textbf{CPP option} & \textbf{Description} \\ |
70 |
\hline \hline |
\hline \hline |
71 |
\texttt{ALLOW\_OBCS\_NORTH} & |
\code{ALLOW\_OBCS\_NORTH} & |
72 |
enable Northern OB \\ |
enable Northern OB \\ |
73 |
\texttt{ALLOW\_OBCS\_SOUTH} & |
\code{ALLOW\_OBCS\_SOUTH} & |
74 |
enable Southern OB \\ |
enable Southern OB \\ |
75 |
\texttt{ALLOW\_OBCS\_EAST} & |
\code{ALLOW\_OBCS\_EAST} & |
76 |
enable Eastern OB \\ |
enable Eastern OB \\ |
77 |
\texttt{ALLOW\_OBCS\_WEST} & |
\code{ALLOW\_OBCS\_WEST} & |
78 |
enable Western OB \\ |
enable Western OB \\ |
79 |
\hline |
\hline |
80 |
\texttt{ALLOW\_OBCS\_PRESCRIBE} & |
\code{ALLOW\_OBCS\_PRESCRIBE} & |
81 |
enable code for prescribing OB's \\ |
enable code for prescribing OB's \\ |
82 |
\texttt{ALLOW\_OBCS\_SPONGE} & |
\code{ALLOW\_OBCS\_SPONGE} & |
83 |
enable sponge layer code \\ |
enable sponge layer code \\ |
84 |
\texttt{ALLOW\_OBCS\_BALANCE} & |
\code{ALLOW\_OBCS\_BALANCE} & |
85 |
enable code for balancing transports through OB's \\ |
enable code for balancing transports through OB's \\ |
86 |
\texttt{ALLOW\_ORLANSKI} & |
\code{ALLOW\_ORLANSKI} & |
87 |
enable Orlanski radiation conditions at OB's \\ |
enable Orlanski radiation conditions at OB's \\ |
88 |
|
\code{ALLOW\_OBCS\_STEVENS} & |
89 |
|
enable Stevens (1990) boundary conditions at OB's \\ |
90 |
|
& (currently only implemented for eastern and western \\ |
91 |
|
& boundaries and NOT for ptracers) \\ |
92 |
\hline |
\hline |
93 |
\end{tabular} |
\end{tabular} |
94 |
} |
} |
102 |
\label{sec:pkg:obcs:runtime}} |
\label{sec:pkg:obcs:runtime}} |
103 |
|
|
104 |
Run-time parameters are set in files |
Run-time parameters are set in files |
105 |
\texttt{data.pkg}, \texttt{data.obcs}, and \texttt{data.exf} |
\code{data.pkg}, \code{data.obcs}, and \code{data.exf} |
106 |
if ``real-time'' prescription is requested |
if ``real-time'' prescription is requested |
107 |
(i.e. package \texttt{exf} enabled). |
(i.e. package \code{exf} enabled). |
108 |
These parameter files are read in S/R |
vThese parameter files are read in S/R |
109 |
\texttt{packages\_readparms.F}, \texttt{obcs\_readparms.F}, and |
\code{packages\_readparms.F}, \code{obcs\_readparms.F}, and |
110 |
\texttt{exf\_readparms.F}, respectively. |
\code{exf\_readparms.F}, respectively. |
111 |
Run-time parameters may be broken into 3 categories: |
Run-time parameters may be broken into 3 categories: |
112 |
(i) switching on/off the package at runtime, |
(i) switching on/off the package at runtime, |
113 |
(ii) OBCS package flags and parameters, |
(ii) OBCS package flags and parameters, |
114 |
(iii) additional timing flags in \texttt{data.exf}, if selected. |
(iii) additional timing flags in \code{data.exf}, if selected. |
115 |
|
|
116 |
\paragraph{Enabling the package} |
\paragraph{Enabling the package} |
117 |
~ \\ |
~ \\ |
118 |
% |
% |
119 |
The OBCS package is switched on at runtime by setting |
The OBCS package is switched on at runtime by setting |
120 |
\texttt{useOBCS = .TRUE.} in \texttt{data.pkg}. |
\code{useOBCS = .TRUE.} in \code{data.pkg}. |
121 |
|
|
122 |
\paragraph{Package flags and parameters} |
\paragraph{Package flags and parameters} |
123 |
~ \\ |
~ \\ |
124 |
% |
% |
125 |
Table \ref{tab:pkg:obcs:runtime_flags} summarizes the |
Table \ref{tab:pkg:obcs:runtime_flags} summarizes the |
126 |
runtime flags that are set in \texttt{data.obcs}, and |
runtime flags that are set in \code{data.obcs}, and |
127 |
their default values. |
their default values. |
128 |
|
|
129 |
\begin{table}[!ht] |
\begin{table}[!ht] |
133 |
\hline |
\hline |
134 |
\textbf{Flag/parameter} & \textbf{default} & \textbf{Description} \\ |
\textbf{Flag/parameter} & \textbf{default} & \textbf{Description} \\ |
135 |
\hline \hline |
\hline \hline |
136 |
\multicolumn{3}{|c|}{\textit{basic flags \& parameters} } \\ |
\multicolumn{3}{|c|}{\textit{basic flags \& parameters} (OBCS\_PARM01) } \\ |
137 |
\hline |
\hline |
138 |
OB\_Jnorth & 0 & |
OB\_Jnorth & 0 & |
139 |
Nx-vector of J-indices (w.r.t. Ny) of Northern OB |
Nx-vector of J-indices (w.r.t. Ny) of Northern OB |
147 |
OB\_Iwest & 0 & |
OB\_Iwest & 0 & |
148 |
Ny-vector of I-indices (w.r.t. Nx) of Western OB |
Ny-vector of I-indices (w.r.t. Nx) of Western OB |
149 |
at each J-position (w.r.t. Ny) \\ |
at each J-position (w.r.t. Ny) \\ |
150 |
useOBCSprescribe & \texttt{.FALSE.} & |
useOBCSprescribe & \code{.FALSE.} & |
151 |
~ \\ |
~ \\ |
152 |
useOBCSsponge & \texttt{.FALSE.} & |
useOBCSsponge & \code{.FALSE.} & |
153 |
~ \\ |
~ \\ |
154 |
useOBCSbalance & \texttt{.FALSE.} & |
useOBCSbalance & \code{.FALSE.} & |
155 |
~ \\ |
~ \\ |
156 |
|
OBCS\_balanceFacN/S/E/W & 1 & factor(s) determining the details |
157 |
|
of the balaning code \\ |
158 |
|
useOrlanskiNorth/South/EastWest & \code{.FALSE.} & |
159 |
|
turn on Orlanski boundary conditions for individual boundary\\ |
160 |
|
useStevensNorth/South/EastWest & \code{.FALSE.} & |
161 |
|
turn on Stevens boundary conditions for individual boundary\\ |
162 |
OB\textbf{X}\textbf{y}File & ~ & |
OB\textbf{X}\textbf{y}File & ~ & |
163 |
file name of OB field \\ |
file name of OB field \\ |
164 |
~ & ~ & |
~ & ~ & |
166 |
\textbf{E}(ast), \textbf{W}(est) \\ |
\textbf{E}(ast), \textbf{W}(est) \\ |
167 |
~ & ~ & |
~ & ~ & |
168 |
\textbf{y}: \textbf{t}(emperature), \textbf{s}(salinity), |
\textbf{y}: \textbf{t}(emperature), \textbf{s}(salinity), |
169 |
\textbf{u}(-velocity), \textbf{v}(-velocity) \\ |
\textbf{u}(-velocity), \textbf{v}(-velocity), \\ |
170 |
|
~ & ~ & |
171 |
|
\textbf{w}(-velocity), \textbf{eta}(sea surface height)\\ |
172 |
|
~ & ~ & |
173 |
|
\textbf{a}(sea ice area), \textbf{h}(sea ice thickness), |
174 |
|
\textbf{sn}(snow thickness), \textbf{sl}(sea ice salinity)\\ |
175 |
\hline |
\hline |
176 |
\multicolumn{3}{|c|}{\textit{Orlanski parameters} } \\ |
\multicolumn{3}{|c|}{\textit{Orlanski parameters} (OBCS\_PARM02) } \\ |
177 |
\hline |
\hline |
178 |
cvelTimeScale & 2000 sec & |
cvelTimeScale & 2000 sec & |
179 |
averaging period for phase speed \\ |
averaging period for phase speed \\ |
181 |
maximum allowable phase speed-CFL for AB-II \\ |
maximum allowable phase speed-CFL for AB-II \\ |
182 |
CFIX & 0.8 m/s & |
CFIX & 0.8 m/s & |
183 |
fixed boundary phase speed \\ |
fixed boundary phase speed \\ |
184 |
useFixedCEast & .FALSE. & |
useFixedCEast & \code{.FALSE.} & |
185 |
~ \\ |
~ \\ |
186 |
useFixedCWest & .FALSE. & |
useFixedCWest & \code{.FALSE.} & |
187 |
~ \\ |
~ \\ |
188 |
\hline |
\hline |
189 |
\multicolumn{3}{|c|}{\textit{Sponge-layer parameters} } \\ |
\multicolumn{3}{|c|}{\textit{Sponge-layer parameters} (OBCS\_PARM03)} \\ |
190 |
\hline |
\hline |
191 |
spongeThickness & 0 & |
spongeThickness & 0 & |
192 |
sponge layer thickness (in \# grid points) \\ |
sponge layer thickness (in \# grid points) \\ |
202 |
Vrelaxobcsbound & 0 sec & |
Vrelaxobcsbound & 0 sec & |
203 |
relaxation time scale at the |
relaxation time scale at the |
204 |
outermost sponge layer point of a zonal OB \\ |
outermost sponge layer point of a zonal OB \\ |
205 |
|
\hline |
206 |
|
\multicolumn{3}{|c|}{\textit{Stevens parameters} (OBCS\_PARM04) } \\ |
207 |
|
\hline |
208 |
|
T/SrelaxStevens & 0~sec & relaxation time scale for |
209 |
|
temperature/salinity \\ |
210 |
|
useStevensPhaseVel & \code{.TRUE.} & \\ |
211 |
|
useStevensAdvection & \code{.TRUE.} & \\ |
212 |
\hline |
\hline |
213 |
\hline |
\hline |
214 |
\end{tabular} |
\end{tabular} |
228 |
Northern, Southern, Eastern, and Western. |
Northern, Southern, Eastern, and Western. |
229 |
All OB locations are specified by their absolute |
All OB locations are specified by their absolute |
230 |
meridional (Northern/Southern) or zonal (Eastern/Western) indices. |
meridional (Northern/Southern) or zonal (Eastern/Western) indices. |
231 |
Thus, for each zonal position $i=1,\ldots,Nx$ a meridional index |
Thus, for each zonal position $i=1,\ldots,N_x$ a meridional index |
232 |
$j$ specifies the Northern/Southern OB position, |
$j$ specifies the Northern/Southern OB position, |
233 |
and for each meridional position $j=1,\ldots,Ny$, a zonal index |
and for each meridional position $j=1,\ldots,N_y$, a zonal index |
234 |
$i$ specifies the Eastern/Western OB position. |
$i$ specifies the Eastern/Western OB position. |
235 |
For Northern/Southern OB this defines an $Nx$-dimensional |
For Northern/Southern OB this defines an $N_x$-dimensional |
236 |
``row'' array $\tt OB\_Jnorth(Ny)$ / $\tt OB\_Jsouth(Ny)$, |
``row'' array $\tt OB\_Jnorth(Nx)$ / $\tt OB\_Jsouth(Nx)$, |
237 |
and an $Ny$-dimenisonal |
and an $N_y$-dimenisonal |
238 |
``column'' array $\tt OB\_Ieast(Nx)$ / $\tt OB\_Iwest(Nx)$ |
``column'' array $\tt OB\_Ieast(Ny)$ / $\tt OB\_Iwest(Ny)$. |
239 |
Positions determined in this way allows Northern/Southern |
Positions determined in this way allows Northern/Southern |
240 |
OBs to be at variable $j$ (or $y$) positions, and Eastern/Western |
OBs to be at variable $j$ (or $y$) positions, and Eastern/Western |
241 |
OBs at variable $i$ (or $x$) positions. |
OBs at variable $i$ (or $x$) positions. |
244 |
means there is no corresponding OB in that column/row. |
means there is no corresponding OB in that column/row. |
245 |
For a Northern/Southern OB, the OB V point is to the South/North. |
For a Northern/Southern OB, the OB V point is to the South/North. |
246 |
For an Eastern/Western OB, the OB U point is to the West/East. |
For an Eastern/Western OB, the OB U point is to the West/East. |
247 |
|
For example, |
248 |
\begin{verbatim} |
\begin{tabbing} |
249 |
For example |
\code{OB\_Jnorth(3)=34} \= means that: \= \\ |
250 |
OB_Jnorth(3)=34 means that: |
\> \code{T(3,34)} \> is a an OB point \\ |
251 |
T( 3 ,34) is a an OB point |
\> \code{U(3,34)} \> is a an OB point \\ |
252 |
U(3:4,34) is a an OB point |
\> \code{V(3,34)} \> is a an OB point \\ |
253 |
V( 4 ,34) is a an OB point |
\code{OB\_Jsouth(3)=1} \> means that: \\ |
254 |
while |
\> \code{T(3,1)} \> is a an OB point \\ |
255 |
OB_Jsouth(3)=1 means that: |
\> \code{U(3,1)} \> is a an OB point \\ |
256 |
T( 3 ,1) is a an OB point |
\> \code{V(3,2)} \> is a an OB point \\ |
257 |
U(3:4,1) is a an OB point |
\code{OB\_Ieast(10)=69} \> means that: \> \\ |
258 |
V( 4 ,2) is a an OB point |
\> \code{T(69,10)} \> is a an OB point \\ |
259 |
\end{verbatim} |
\> \code{U(69,10)} \> is a an OB point \\ |
260 |
|
\> \code{V(69,10)} \> is a an OB point \\ |
261 |
For convenience, negative values for Jnorth/Ieast refer to |
\code{OB\_Iwest(10)=1} \> means that: \> \\ |
262 |
|
\> \code{T(1,10)} \> is a an OB point \\ |
263 |
|
\> \code{U(2,10)} \> is a an OB point \\ |
264 |
|
\> \code{V(1,10)} \> is a an OB point |
265 |
|
\end{tabbing} |
266 |
|
For convenience, negative values for \code{Jnorth}/\code{Ieast} refer to |
267 |
points relative to the Northern/Eastern edges of the model |
points relative to the Northern/Eastern edges of the model |
268 |
eg. $\tt OB\_Jnorth(3)=-1$ means that the point $\tt (3,Ny)$ |
eg. $\tt OB\_Jnorth(3)=-1$ means that the point $\tt (3,Ny)$ |
269 |
is a northern OB. |
is a northern OB. |
279 |
|
|
280 |
\paragraph{OBCS\_READPARMS:} ~ \\ |
\paragraph{OBCS\_READPARMS:} ~ \\ |
281 |
Set OB positions through arrays |
Set OB positions through arrays |
282 |
{\tt OB\_Jnorth(Ny), OB\_Jsouth(Ny), OB\_Ieast(Nx), OB\_Iwest(Nx)}, |
{\tt OB\_Jnorth(Nx), OB\_Jsouth(Nx), OB\_Ieast(Ny), OB\_Iwest(Ny)}, |
283 |
and runtime flags (see Table \ref{tab:pkg:obcs:runtime_flags}). |
and runtime flags (see Table \ref{tab:pkg:obcs:runtime_flags}). |
284 |
|
|
285 |
\paragraph{OBCS\_CALC:} ~ \\ |
\paragraph{OBCS\_CALC:} ~ \\ |
304 |
\item |
\item |
305 |
prescribed time-constant or time-varying fields (see below). |
prescribed time-constant or time-varying fields (see below). |
306 |
% |
% |
307 |
|
\item |
308 |
|
use prescribed boundary fields to compute Stevens boundary conditions. |
309 |
\end{itemize} |
\end{itemize} |
310 |
|
|
311 |
|
\paragraph{ORLANSKI:} ~ \\ |
|
\paragraph{ORLANSKI} ~ \\ |
|
|
% |
|
|
Orlanski radiation conditions \citep{orl:76} |
|
|
|
|
|
\paragraph{OBCS\_PRESCRIBE\_READ} Setting OB fields and updates \\ |
|
312 |
% |
% |
313 |
~ |
Orlanski radiation conditions \citep{orl:76}, examples can be found in |
314 |
|
\code{verification/dome} and |
315 |
|
\code{verification/tutorial\_plume\_on\_slope} |
316 |
|
(\ref{sec:eg-gravityplume}). |
317 |
|
|
318 |
|
\paragraph{OBCS\_PRESCRIBE\_READ:} ~ \\ |
319 |
|
% |
320 |
|
When \code{useOBCSprescribe = .TRUE.} the model tries to read |
321 |
|
temperature, salinity, u- and v-velocities from files specified in the |
322 |
|
runtime parameters \code{OB[N/S/E/W][t/s/u/v]File}. These files are |
323 |
|
the usual IEEE, big-endian files with dimensions of a section along an |
324 |
|
open boundary: |
325 |
|
\begin{itemize} |
326 |
|
\item For North/South boundary files the dimensions are |
327 |
|
$(N_x\times N_r\times\mbox{time levels})$, for East/West boundary |
328 |
|
files the dimensions are $(N_y\times N_r\times\mbox{time levels})$. |
329 |
|
\item If a non-linear free surface is used |
330 |
|
(\ref{sec:nonlinear-freesurface}), additional files |
331 |
|
\code{OB[N/S/E/W]etaFile} for the sea surface height $\eta$ with |
332 |
|
dimension $(N_{x/y}\times\mbox{time levels})$ may be specified. |
333 |
|
\item If non-hydrostatic dynamics are used |
334 |
|
(\ref{sec:non-hydrostatic}), additional files |
335 |
|
\code{OB[N/S/E/W]wFile} for the vertical velocity $w$ with |
336 |
|
dimensions $(N_{x/y}\times N_r\times\mbox{time levels})$ can be |
337 |
|
specified. |
338 |
|
\item If \code{useSEAICE=.TRUE.} then additional files |
339 |
|
\code{OB[N/S/E/W][a,h,sl,sn,uice,vice]} for sea ice area, thickness |
340 |
|
(\code{HEFF}), seaice salinity, snow and ice velocities |
341 |
|
$(N_{x/y}\times\mbox{time levels})$ can be specified. |
342 |
|
\end{itemize} |
343 |
|
As in \code{S/R external\_fields\_load} or the \code{exf}-package, the |
344 |
|
code reads two time levels for each variable, e.g.\ \code{OBNu0} and |
345 |
|
\code{OBNu1}, and interpolates linearly between these time levels to |
346 |
|
obtain the value \code{OBNu} at the current model time (step). When the |
347 |
|
\code{exf}-package is used, the time levels are controlled for each |
348 |
|
boundary separately in the same way as the \code{exf}-fields in |
349 |
|
\code{data.exf}, namelist \code{EXF\_NML\_OBCS}. The runtime flags |
350 |
|
follow the above naming conventions, e.g. for the western boundary the |
351 |
|
corresponding flags are \code{OBCWstartdate1/2} and |
352 |
|
\code{OBCWperiod}. Sea-ice boundary values are controlled separately |
353 |
|
with \code{siobWstartdate1/2} and \code{siobWperiod}. When the |
354 |
|
\code{exf}-package is not used, the time levels are controlled by the |
355 |
|
runtime flags \code{externForcingPeriod} and \code{externForcingCycle} |
356 |
|
in \code{data}, see \code{verification/exp4} for an example. |
357 |
|
|
358 |
|
\paragraph{OBCS\_CALC\_STEVENS:} ~ \\ |
359 |
|
(THE IMPLEMENTATION OF THESE BOUNDARY CONDITIONS IS NOT |
360 |
|
COMPLETE. PASSIVE TRACERS, SEA ICE AND NON-LINEAR FREE SURFACE ARE NOT |
361 |
|
SUPPORTED PROPERLY.) \\ |
362 |
|
The boundary conditions following \citet{stevens:90} require the |
363 |
|
vertically averaged normal velocity (originally specified as a stream |
364 |
|
function along the open boundary) $\bar{u}_{ob}$ and the tracer fields |
365 |
|
$\chi_{ob}$ (note: passive tracers are currently not implemented and |
366 |
|
the code stops when package \code{ptracers} is used together with this |
367 |
|
option). Currently, the code vertically averages the normal velocity |
368 |
|
as specified in \code{OB[E,W]u} or \code{OB[N,S]v}. From these |
369 |
|
prescribed values the code computes the boundary values for the next |
370 |
|
timestep $n+1$ as follows (as an example, we use the notation for an |
371 |
|
eastern or western boundary): |
372 |
|
\begin{itemize} |
373 |
|
\item $u^{n+1}(y,z) = \bar{u}_{ob}(y) + (u')^{n}(y,z)$, where |
374 |
|
$(u')^{n}$ is the deviation from the vertically averaged velocity at |
375 |
|
timestep $n$ on the boundary. $(u')^{n}$ is computed in the previous |
376 |
|
time step $n$ from the intermediate velocity $u^*$ prior to the |
377 |
|
correction step (see section \ref{sec:time_stepping}, e.g., |
378 |
|
eq.\,(\ref{eq:ustar-backward-free-surface})). |
379 |
|
% and~(\ref{eq:vstar-backward-free-surface})). |
380 |
|
(This velocity is not |
381 |
|
available at the beginning of the next time step $n+1$, when |
382 |
|
S/R~OBCS\_CALC/OBCS\_CALC\_STEVENS are called, therefore it needs to |
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|
be saved in S/R~DYNAMICS by calling S/R~OBCS\_SAVE\_UV\_N and also |
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stored in a separate restart files |
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\verb+pickup_stevens[N/S/E/W].${iteration}.data+) |
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% Define CPP-flag OBCS\_STEVENS\_USE\_INTERIOR\_VELOCITY to use the |
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% velocity one grid point inward from the boundary. |
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|
\item If $u^{n+1}$ is directed into the model domain, the boudary |
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value for tracer $\chi$ is restored to the prescribed values: |
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\[\chi^{n+1} = \chi^{n} + \frac{\Delta{t}}{\tau_\chi} (\chi_{ob} - |
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|
\chi^{n}),\] where $\tau_\chi$ is the relaxation time |
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scale \texttt{T/SrelaxStevens}. The new $\chi^{n+1}$ is then subject |
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to the advection by $u^{n+1}$. |
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\item If $u^{n+1}$ is directed out of the model domain, the tracer |
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$\chi^{n+1}$ on the boundary at timestep $n+1$ is estimated from |
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advection out of the domain with $u^{n+1}+c$, where $c$ is |
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a phase velocity estimated as |
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$\frac{1}{2}\frac{\partial\chi}{\partial{t}}/\frac{\partial\chi}{\partial{x}}$. The |
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numerical scheme is (as an example for an eastern boundary): |
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|
\[\chi_{i_{b},j,k}^{n+1} = \chi_{i_{b},j,k}^{n} + \Delta{t} |
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(u^{n+1}+c)_{i_{b},j,k}\frac{\chi_{i_{b},j,k}^{n} |
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- \chi_{i_{b}-1,j,k}^{n}}{\Delta{x}_{i_{b},j}^{C}}\mbox{, if }u_{i_{b},j,k}^{n+1}>0, |
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|
\] where $i_{b}$ is the boundary index.\\ |
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For test purposes, the phase velocity contribution or the entire |
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|
advection can be turned off by setting the corresponding parameters |
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|
\texttt{useStevensPhaseVel} and \texttt{useStevensAdvection} to |
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|
\texttt{.FALSE.}. |
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\end{itemize} |
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See \citet{stevens:90} for details. With this boundary condition |
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|
specifying the exact net transport across the open boundary is simple, |
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|
so that balancing the flow with (S/R~OBCS\_BALANCE\_FLOW, see next |
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|
paragraph) is usually not necessary. |
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|
|
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|
\paragraph{OBCS\_BALANCE\_FLOW:} ~ \\ |
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|
% |
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|
When turned on (\code{ALLOW\_OBCS\_BALANCE} |
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|
defined in \code{OBCS\_OPTIONS.h} and \code{useOBCSbalance=.true.} in |
418 |
|
\code{data.obcs/OBCS\_PARM01}), this routine balances the net flow |
419 |
|
across the open boundaries. By default the net flow across the |
420 |
|
boundaries is computed and all normal velocities on boundaries are |
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|
adjusted to obtain zero net inflow. |
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|
|
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|
This behavior can be controlled with the runtime flags |
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|
\code{OBCS\_balanceFacN/S/E/W}. The values of these flags determine |
425 |
|
how the net inflow is redistributed as small correction velocities |
426 |
|
between the individual sections. A value ``\code{-1}'' balances an |
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|
individual boundary, values $>0$ determine the relative size of the |
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|
correction. For example, the values |
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|
\begin{tabbing} |
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|
\code{OBCS\_balanceFacE}\code{ = 1.,} \\ |
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|
\code{OBCS\_balanceFacW}\code{ = -1.,} \\ |
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|
\code{OBCS\_balanceFacN}\code{ = 2.,} \\ |
433 |
|
\code{OBCS\_balanceFacS}\code{ = 0.,} |
434 |
|
\end{tabbing} |
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|
make the model |
436 |
|
\begin{itemize} |
437 |
|
\item correct Western \code{OBWu} by substracting a uniform velocity to |
438 |
|
ensure zero net transport through the Western open boundary; |
439 |
|
\item correct Eastern and Northern normal flow, with the Northern |
440 |
|
velocity correction two times larger than the Eastern correction, but |
441 |
|
\emph{not} the Southern normal flow, to ensure that the total inflow through |
442 |
|
East, Northern, and Southern open boundary is balanced. |
443 |
|
\end{itemize} |
444 |
|
|
445 |
\paragraph{OBCS\_BALANCE} ~ \\ |
The old method of balancing the net flow for all sections individually |
446 |
% |
can be recovered by setting all flags to -1. Then the normal |
447 |
~ |
velocities across each of the four boundaries are modified separately, |
448 |
|
so that the net volume transport across \emph{each} boundary is |
449 |
|
zero. For example, for the western boundary at $i=i_{b}$, the modified |
450 |
|
velocity is: |
451 |
|
\[ |
452 |
|
u(y,z) - \int_{\mbox{western boundary}}u\,dy\,dz \approx OBNu(j,k) - \sum_{j,k} |
453 |
|
OBNu(j,k) h_{w}(i_{b},j,k)\Delta{y_G(i_{b},j)}\Delta{z(k)}. |
454 |
|
\] |
455 |
|
This also ensures a net total inflow of zero through all boundaries, |
456 |
|
but this combination of flags is \emph{not} useful if you want to |
457 |
|
simulate, say, a sector of the Southern Ocean with a strong ACC |
458 |
|
entering through the western and leaving through the eastern boundary, |
459 |
|
because the value of ``\code{-1}'' for these flags will make sure that |
460 |
|
the strong inflow is removed. Clearly, gobal balancing with |
461 |
|
\code{OBCS\_balanceFacE/W/N/S} $\ge0$ is the preferred method. |
462 |
|
|
463 |
\paragraph{OBCS\_APPLY\_*:} ~ \\ |
\paragraph{OBCS\_APPLY\_*:} ~ \\ |
464 |
~ |
~ |
465 |
|
|
466 |
\paragraph{OBCS\_SPONGE} Setting sponge layer characteristics \\ |
\paragraph{OBCS\_SPONGE:} ~ \\ |
467 |
% |
% |
468 |
~ |
The sponge layer code (turned on with \code{ALLOW\_OBCS\_SPONGE} and |
469 |
|
\code{useOBCSsponge}) adds a relaxation term to the right-hand-side of |
470 |
|
the momentum and tracer equations. The variables are relaxed towards |
471 |
|
the boundary values with a relaxation time scale that increases |
472 |
|
linearly with distance from the boundary |
473 |
|
\[ |
474 |
|
G_{\chi}^{\mbox{(sponge)}} = |
475 |
|
- \frac{\chi - [( L - \delta{L} ) \chi_{BC} + \delta{L}\chi]/L} |
476 |
|
{[(L-\delta{L})\tau_{b}+\delta{L}\tau_{i}]/L} |
477 |
|
= - \frac{\chi - [( 1 - l ) \chi_{BC} + l\chi]} |
478 |
|
{[(1-l)\tau_{b}+l\tau_{i}]} |
479 |
|
\] |
480 |
|
where $\chi$ is the model variable (U/V/T/S) in the interior, |
481 |
|
$\chi_{BC}$ the boundary value, $L$ the thickness of the sponge layer |
482 |
|
(runtime parameter \code{spongeThickness} in number of grid points), |
483 |
|
$\delta{L}\in[0,L]$ ($\frac{\delta{L}}{L}=l\in[0,1]$) the distance from the boundary (also in grid points), and |
484 |
|
$\tau_{b}$ (runtime parameters \code{Urelaxobcsbound} and |
485 |
|
\code{Vrelaxobcsbound}) and $\tau_{i}$ (runtime parameters |
486 |
|
\code{Urelaxobcsinner} and \code{Vrelaxobcsinner}) the relaxation time |
487 |
|
scales on the boundary and at the interior termination of the sponge |
488 |
|
layer. The parameters \code{Urelaxobcsbound/inner} set the relaxation |
489 |
|
time scales for the Eastern and Western boundaries, |
490 |
|
\code{Vrelaxobcsbound/inner} for the Northern and Southern boundaries. |
491 |
|
|
492 |
\paragraph{OB's with nonlinear free surface} ~ \\ |
\paragraph{OB's with nonlinear free surface} ~ \\ |
493 |
% |
% |
536 |
%---------------------------------------------------------------------- |
%---------------------------------------------------------------------- |
537 |
|
|
538 |
\subsubsection{Reference experiments} |
\subsubsection{Reference experiments} |
539 |
|
In the directory \code{verifcation}, the following experiments use |
540 |
|
\code{obcs}: |
541 |
|
\begin{itemize} |
542 |
|
\item \code{exp4}: box with 4 open boundaries, simulating flow over a |
543 |
|
Gaussian bump based on \citet{adcroft:97}, also tests |
544 |
|
Stevens-boundary conditions; |
545 |
|
\item \code{dome}: based on the project ``Dynamics of Overflow Mixing |
546 |
|
and Entrainment'' |
547 |
|
(\url{http://www.rsmas.miami.edu/personal/tamay/DOME/dome.html}), uses |
548 |
|
Orlanski-BCs; |
549 |
|
\item \code{internal\_wave}: uses a heavily modified \code{S/R~OBCS\_CALC} |
550 |
|
\item \code{seaice\_obcs}: simple example who to use the sea-ice |
551 |
|
related code, based on \code{lab\_sea}; |
552 |
|
\item \code{tutorial\_plume\_on\_slope}: uses Orlanski-BCs, see also |
553 |
|
section~\ref{sec:eg-gravityplume}. |
554 |
|
\end{itemize} |
555 |
|
|
556 |
|
|
557 |
|
|
563 |
\label{sec:pkg:obcs:experiments} |
\label{sec:pkg:obcs:experiments} |
564 |
|
|
565 |
\begin{itemize} |
\begin{itemize} |
566 |
\item{Ocean experiment in exp4 verification directory. } |
\item \code{tutorial\_plume\_on\_slope} (section~\ref{sec:eg-gravityplume}) |
567 |
\end{itemize} |
\end{itemize} |
568 |
|
|
569 |
|
|
570 |
|
%%% Local Variables: |
571 |
|
%%% mode: latex |
572 |
|
%%% TeX-master: "../../manual" |
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%%% End: |