PHC_60 run

This run is based on the PHC_49 one except that:

• decrease by 15% runoffs beyond 65°N in sbcrnf.F90
  

Few patterns list:

- This experiment is not convincing at all since there is no changes

# Freshwater budget after 10 years

Bilan (Sv) en moyenne annuelle pour l"experience:  PHC60
                                
           Precip  :      12.567102
 NOT modif Runoff  :       1.2773800
     modif Runoff  :       1.2322448   (decrease by  0.0167 Sv / PHC_49)
           ErP     :      -0.50366824  (decrease by -0.0211 Sv / PHC_49)
           EmPold  :       0.0000000
           SSH mean:       0.21261765
           -----------------------------
           EmP     :      -0.027508610

Evap a partir du flux Qla (pour information, non utilisee) : Evap_Svqla = 13.732051 Sv
Evap a partir des termes EmP, precip, ErP, runoff et EmPold: Evap_sv    = 14.275506 Sv

Bilan gain .vs. perte:
           Precip+Runoff_MOD : 13.799346 Sv
           Evap+ErP+EmPold   : 13.771838 Sv

# Time series over 20 years

# Year 10

Temperature differences at z=105 m with Levitus and PHC_49:

Salinity differences at z=105 m with Levitus and PHC_49:

SST differences with Reynolds and PHC_49:

SSS differences with Levitus and PHC_49:

Temperature differences in zonal average with Levitus and PHC_49:

Salinity differences in zonal average with Levitus and PHC_49:

Equatorial differences with Levitus and PHC_49 of zonal velocity U:

Equatorial differences with Levitus and PHC_49 of temperature:

Equatorial differences with Levitus and PHC_49 of salinity:

Pacific equatorial differences with Levitus and PHC_49 of temperature:

Mxl10 differences with PHC_49 :

Qnet differences with PHC_49 :

MHT:

Global MOC:

Atlantic MOC:

BSF:

Erp field:

Zonal Mxl field:

Temperature & Salinity horizontal mean :

Straits transport: