PHC_56 run

This run is based on the PHC_49 one except that:

• nn_fwb = 2 (new case)
  
• correction of the empold from the previous year as follows :
  

# if empold >0 it means that the SSH increase and so imply too much precipitation so empold is spread over erp >0 area to increase evaporation
# if empold <0 it means that the SSH decrease and so imply too much evaporation so empold is spread over erp <0 area to increase precipitation

Few patterns list:

# Freshwater budget after 10 years

# 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: