| 1 |
adcroft |
1.9 |
C $Header: /u/gcmpack/models/MITgcmUV/model/inc/FFIELDS.h,v 1.8 2000/11/13 16:32:57 heimbach Exp $ |
| 2 |
cnh |
1.1 |
C |
| 3 |
|
|
C /==========================================================\ |
| 4 |
|
|
C | FFIELDS.h | |
| 5 |
|
|
C | o Model forcing fields | |
| 6 |
|
|
C |==========================================================| |
| 7 |
|
|
C | The arrays here will need changing and customising for a | |
| 8 |
|
|
C | particular experiment. | |
| 9 |
|
|
C \==========================================================/ |
| 10 |
|
|
C |
| 11 |
|
|
C-- For a classical "gyre" type experiment just one term is needed. |
| 12 |
heimbach |
1.7 |
C |
| 13 |
adcroft |
1.9 |
C fu - Zonal surface wind stress |
| 14 |
|
|
C Units are N/m^2 (>0 from East to West) |
| 15 |
|
|
C |
| 16 |
|
|
C fv - Meridional surface wind stress |
| 17 |
|
|
C Units are N/m^2 (>0 from North to South)) |
| 18 |
heimbach |
1.7 |
C |
| 19 |
|
|
C EmPmR - Evaporation - Precipitation - Runoff |
| 20 |
adcroft |
1.9 |
C Units are m/s (>0 for ocean salting) |
| 21 |
|
|
C |
| 22 |
|
|
C Qnet - Upward surface heat flux |
| 23 |
|
|
C Units are W/m^2=kg/s^3 (>0 for ocean cooling) |
| 24 |
|
|
C |
| 25 |
|
|
C Qsw - Upward short-wave surface heat flux |
| 26 |
|
|
C Units are W/m^2=kg/s^3 (>0 for ocean cooling) |
| 27 |
heimbach |
1.7 |
C |
| 28 |
adcroft |
1.6 |
C SST - Sea surface temperature (degrees) for relaxation |
| 29 |
|
|
C SSS - Sea surface salinity (psu) for relaxation |
| 30 |
heimbach |
1.7 |
|
| 31 |
adcroft |
1.4 |
COMMON /FFIELDS/ |
| 32 |
adcroft |
1.6 |
& fu, |
| 33 |
|
|
& fv, |
| 34 |
|
|
& Qnet, |
| 35 |
|
|
& EmPmR, |
| 36 |
|
|
& SST, |
| 37 |
|
|
& SSS, |
| 38 |
|
|
& Qsw |
| 39 |
cnh |
1.3 |
_RS fu (1-OLx:sNx+OLx,1-OLy:sNy+OLy,nSx,nSy) |
| 40 |
|
|
_RS fv (1-OLx:sNx+OLx,1-OLy:sNy+OLy,nSx,nSy) |
| 41 |
adcroft |
1.6 |
_RS Qnet (1-OLx:sNx+OLx,1-OLy:sNy+OLy,nSx,nSy) |
| 42 |
|
|
_RS EmPmR (1-OLx:sNx+OLx,1-OLy:sNy+OLy,nSx,nSy) |
| 43 |
adcroft |
1.4 |
_RS SST (1-OLx:sNx+OLx,1-OLy:sNy+OLy,nSx,nSy) |
| 44 |
|
|
_RS SSS (1-OLx:sNx+OLx,1-OLy:sNy+OLy,nSx,nSy) |
| 45 |
adcroft |
1.6 |
_RS Qsw (1-OLx:sNx+OLx,1-OLy:sNy+OLy,nSx,nSy) |
| 46 |
heimbach |
1.7 |
|
| 47 |
adcroft |
1.9 |
C surfaceTendencyU (units are m/s^2) |
| 48 |
heimbach |
1.7 |
C -> usage in gU: gU = gU + surfaceTendencyU[m/s^2] |
| 49 |
|
|
C |
| 50 |
adcroft |
1.9 |
C surfaceTendencyV (units are m/s^2) |
| 51 |
heimbach |
1.7 |
C -> usage in gV: gV = gV + surfaceTendencyV[m/s^2] |
| 52 |
|
|
C |
| 53 |
adcroft |
1.9 |
C surfaceTendencyS (units are psu/s) |
| 54 |
heimbach |
1.7 |
C - EmPmR plus salinity relaxation term |
| 55 |
|
|
C -> calculate -lambda*(S(model)-S(clim)) |
| 56 |
|
|
C -> usage in gS: gS = gS + surfaceTendencyS[psu/s] |
| 57 |
|
|
C |
| 58 |
adcroft |
1.9 |
C surfaceTendencyT (units are degrees/s) |
| 59 |
heimbach |
1.7 |
C - Qnet plus temp. relaxation |
| 60 |
|
|
C -> calculate -lambda*(T(model)-T(clim)) |
| 61 |
|
|
C >>> Qnet assumed to be total flux minus s/w rad. <<< |
| 62 |
|
|
C -> usage in gT: gT = gT + surfaceTendencyT[K/s] |
| 63 |
heimbach |
1.8 |
C |
| 64 |
heimbach |
1.7 |
COMMON /TENDENCY_FORCING/ |
| 65 |
|
|
& surfaceTendencyU, |
| 66 |
|
|
& surfaceTendencyV, |
| 67 |
|
|
& surfaceTendencyT, |
| 68 |
heimbach |
1.8 |
& surfaceTendencyS, |
| 69 |
|
|
& tempQsw |
| 70 |
heimbach |
1.7 |
_RS surfaceTendencyU (1-OLx:sNx+OLx,1-OLy:sNy+OLy,nSx,nSy) |
| 71 |
|
|
_RS surfaceTendencyV (1-OLx:sNx+OLx,1-OLy:sNy+OLy,nSx,nSy) |
| 72 |
|
|
_RS surfaceTendencyT (1-OLx:sNx+OLx,1-OLy:sNy+OLy,nSx,nSy) |
| 73 |
|
|
_RS surfaceTendencyS (1-OLx:sNx+OLx,1-OLy:sNy+OLy,nSx,nSy) |
| 74 |
heimbach |
1.8 |
_RS tempQsw (1-OLx:sNx+OLx,1-OLy:sNy+OLy,nSx,nSy) |
Parent Directory
| 
Revision Log
| 
Revision Graph