| 9 |
C \==========================================================/ |
C \==========================================================/ |
| 10 |
C |
C |
| 11 |
C-- For a classical "gyre" type experiment just one term is needed. |
C-- For a classical "gyre" type experiment just one term is needed. |
| 12 |
C fu - Zonal velocity tendency term ( m/s^2 ) |
C |
| 13 |
C fv - Meridional velocity tendency term ( m/s^2 ) |
C fu - Zonal velocity tendency term |
| 14 |
C Qnet - Surface heat flux (converted to degrees/second) |
C -> read assumes N/m^2 (>0 from East to West) |
| 15 |
C EmPmR - Evaporation - Precipitation - Runoff (converted to psu/second) |
C -> transformed to m/s^2 |
| 16 |
|
C via fu -> fu/(rhoNil*dR) |
| 17 |
|
C -> usage in gU: gU = gU + fu[m/s^2] |
| 18 |
|
C |
| 19 |
|
C fv - Meridional velocity tendency term |
| 20 |
|
C -> read assumes N/m^2 (>0 from North to South)) |
| 21 |
|
C -> transformed to m/s^2 |
| 22 |
|
C via fv -> fv/(rhoNil*dR) |
| 23 |
|
C -> usage in gU: gV = gV + fu[m/s^2] |
| 24 |
|
C |
| 25 |
|
C EmPmR - Evaporation - Precipitation - Runoff |
| 26 |
|
C -> read assumes m/s (>0 for ocean salting) |
| 27 |
|
C -> transformed to psu/s |
| 28 |
|
C via empmr -> -empmr*35./dR |
| 29 |
|
C -> usage in gS: gS = gS + empmr[psu/s] |
| 30 |
|
C |
| 31 |
|
C Qnet - Surface heat flux |
| 32 |
|
C -> read assumes W/m^2=kg/s^3 (>0 for ocean cooling) |
| 33 |
|
C -> transformed to K/s |
| 34 |
|
C via Qnet -> -Qnet/(rhonil*Cp*dR) |
| 35 |
|
C -> usage in gT: gT = gT + qnet[K/s] |
| 36 |
|
C |
| 37 |
|
C Qsw - Short-wave surface heat flux |
| 38 |
|
C -> read assumes W/m^2=kg/s^3 (>0 for ocean cooling) |
| 39 |
|
C -> transformed to K/s |
| 40 |
|
C via Qsw -> -Qsw/(rhonil*Cp*dR) |
| 41 |
|
C -> usage in gT: gT = gT + Qswt[K/s] |
| 42 |
|
C only for #define SHORTWAVE_HEATING |
| 43 |
|
C |
| 44 |
C SST - Sea surface temperature (degrees) for relaxation |
C SST - Sea surface temperature (degrees) for relaxation |
| 45 |
C SSS - Sea surface salinity (psu) for relaxation |
C SSS - Sea surface salinity (psu) for relaxation |
| 46 |
C Qsw - Short-wave surface heat flux (converted to degrees/second) |
|
| 47 |
COMMON /FFIELDS/ |
COMMON /FFIELDS/ |
| 48 |
& fu, |
& fu, |
| 49 |
& fv, |
& fv, |
| 59 |
_RS SST (1-OLx:sNx+OLx,1-OLy:sNy+OLy,nSx,nSy) |
_RS SST (1-OLx:sNx+OLx,1-OLy:sNy+OLy,nSx,nSy) |
| 60 |
_RS SSS (1-OLx:sNx+OLx,1-OLy:sNy+OLy,nSx,nSy) |
_RS SSS (1-OLx:sNx+OLx,1-OLy:sNy+OLy,nSx,nSy) |
| 61 |
_RS Qsw (1-OLx:sNx+OLx,1-OLy:sNy+OLy,nSx,nSy) |
_RS Qsw (1-OLx:sNx+OLx,1-OLy:sNy+OLy,nSx,nSy) |
| 62 |
|
|
| 63 |
|
C surfaceTendencyU |
| 64 |
|
C -> usage in gU: gU = gU + surfaceTendencyU[m/s^2] |
| 65 |
|
C |
| 66 |
|
C surfaceTendencyV |
| 67 |
|
C -> usage in gV: gV = gV + surfaceTendencyV[m/s^2] |
| 68 |
|
C |
| 69 |
|
C surfaceTendencyS |
| 70 |
|
C - EmPmR plus salinity relaxation term |
| 71 |
|
C -> calculate -lambda*(S(model)-S(clim)) |
| 72 |
|
C -> usage in gS: gS = gS + surfaceTendencyS[psu/s] |
| 73 |
|
C |
| 74 |
|
C surfaceTendencyT |
| 75 |
|
C - Qnet plus temp. relaxation |
| 76 |
|
C -> calculate -lambda*(T(model)-T(clim)) |
| 77 |
|
C >>> Qnet assumed to be total flux minus s/w rad. <<< |
| 78 |
|
C -> usage in gT: gT = gT + surfaceTendencyT[K/s] |
| 79 |
|
|
| 80 |
|
COMMON /TENDENCY_FORCING/ |
| 81 |
|
& surfaceTendencyU, |
| 82 |
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& surfaceTendencyV, |
| 83 |
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& surfaceTendencyT, |
| 84 |
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& surfaceTendencyS |
| 85 |
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_RS surfaceTendencyU (1-OLx:sNx+OLx,1-OLy:sNy+OLy,nSx,nSy) |
| 86 |
|
_RS surfaceTendencyV (1-OLx:sNx+OLx,1-OLy:sNy+OLy,nSx,nSy) |
| 87 |
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_RS surfaceTendencyT (1-OLx:sNx+OLx,1-OLy:sNy+OLy,nSx,nSy) |
| 88 |
|
_RS surfaceTendencyS (1-OLx:sNx+OLx,1-OLy:sNy+OLy,nSx,nSy) |
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