PHC_41 run

This run is based on the PHC_37 one except that: We limit the erp flux to either +6/-6 mm/day
Few patterns list:

- damping term tend to precipitate (strong <0 value for Erp) whereas the volume flux 
correction tend to increase the evaporation
- for instance in areas where ∆SSS is important says >0 for instance, since the volume 
correction EmPold is global, it tends to increase the evaporation process and implies 
a SSS increase and so the ∆SSS differences on so on; the feedback is positive,
there is an amplification of the trend

# Freshwater budget after 10 years

Bilan (Sv) en moyenne annuelle pour l"experience:  PHC41
                                
           Precip  :       11.310391
 NOT modif Runoff  :       1.1496420
     modif Runoff  :       1.1240586
           ErP     :      -1.8750153
           ErP_new :      -1.8179171
           EmPold  :       1.4084227
           -----------------------------
           EmP     :     0.029473463


Evap a partir du flux Qla (pour information, non utilisee) : Evap_Svqla =        13.738964 Sv
Evap a partir des termes EmP, precip, ErP, runoff et EmPold: Evap_sv    =        12.930516 Sv


Bilan gain .vs. perte:

           Precip+Runoff_MOD :       12.434450 Sv
           Evap+ErP+EmPold   :       12.463923 Sv

# Year 10

Temperature differences at z=105 m with Levitus and PHC_37:

Salinity differences at z=105 m with Levitus and PHC_37:

SST differences with Reynolds and PHC_37:

SSS differences with Levitus and PHC_37:

Temperature differences in zonal average with Levitus and PHC_37:

Salinity differences in zonal average with Levitus and PHC_37:

Equatorial differences with Levitus and PHC_37 of zonal velocity U:

Equatorial differences with Levitus and PHC_37 of temperature:

Equatorial differences with Levitus and PHC_37 of salinity:

Pacific equatorial differences with Levitus and PHC_37 of temperature:

Qnet differences with PHC_37 :

MHT:

Global MOC:

Atlantic MOC:

BSF:

Mediterranean water Lat: 40°N, depth 700 m:

Mediterranean water Lat: 38°N, depth 1000 m:

Erp & Mxl fields:

Temperature & Salinity horizontal mean :

Straits transport: