PHC_44 run

This run is based on the PHC_37 one except that:

• nn_fwb=0 no freshwater correction
  
• TKE penetration is fixed to 10% instead 5%

Few patterns list:

- Thermocline warmer than in PHC_37 
- salinity decrease O(-0.1 PSU) at 100 meters all around Antarctica and Arctic bassins
whereas eit increase by O(0.1 PSU) in eastern part of oceans Atlantic and Pacific areas 
good trend relativeli to Levitus 

# Time series over 1000 years

AMOC, AABW cell, DRAKE transport

Sea-ice area

T&S horizontal drift relatively to Levitus [TS]n -[TS]Levitus

T&S horizontal stabilization [TS]n -[TS]final

Kz tides

# Year 10

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

Salinity differences at z=105 m with Levitus and PHC_16:

SST differences with Reynolds and PHC_16:

SSS differences with Levitus and PHC_16:

Temperature differences in zonal average with Levitus and PHC_16:

Salinity differences in zonal average with Levitus and PHC_16:

Equatorial differences with Levitus and PHC_16 of zonal velocity U:

Equatorial differences with Levitus and PHC_16 of temperature:

Equatorial differences with Levitus and PHC_16 of salinity:

Pacific equatorial differences with Levitus and PHC_16 of temperature:

Qnet differences with PHC_16 :

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: