PHC_55 run

This run is based on the PHC_49 one except that:

• nn_fwb = 3 (new case)
  

# if empmean >0 it means that evaporation dominates, so empmean is spread over erp <0 area to increase precipitation
# if empmean <0 it means that precipitation dominates, so empmean is spread over erp >0 area to increase evaporation

Few patterns list:

# Freshwater budget after 10 years

Bilan (Sv) en moyenne annuelle pour l"experience:  PHC55
                                
           Precip  :       12.567102
 NOT modif Runoff  :       1.2773800
     modif Runoff  :       1.2489540
           ErP     :      -1.5274811
           EmPold  :       0.0000000
           SSH mean:      0.65476716
           -----------------------------
           EmP     :     -0.80496445

Evap a partir du flux Qla (pour information, non utilisee) : Evap_Svqla = 13.987346 Sv
Evap a partir des termes EmP, precip, ErP, runoff et EmPold: Evap_sv    = 14.538572 Sv

Bilan gain .vs. perte:
           Precip+Runoff_MOD : 13.816056 Sv
           Evap+ErP+EmPold   : 13.011091 Sv

# Time series over 20 years

# Year 10

Temperature differences at z=105 m with Levitus and PHC_45:

Salinity differences at z=105 m with Levitus and PHC_45:

SST differences with Reynolds and PHC_45:

SSS differences with Levitus and PHC_45:

Temperature differences in zonal average with Levitus and PHC_45:

Salinity differences in zonal average with Levitus and PHC_45:

Equatorial differences with Levitus and PHC_45 of zonal velocity U:

Equatorial differences with Levitus and PHC_45 of temperature:

Equatorial differences with Levitus and PHC_45 of salinity:

Pacific equatorial differences with Levitus and PHC_45 of temperature:

Qnet differences with PHC_45 :

MHT:

Global MOC:

Atlantic MOC:

BSF:

Erp field:

Zonal Mxl field:

Temperature & Salinity horizontal mean :

Straits transport: