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 an increase by O(0.1 PSU) arises in eastern part of Atlantic and Pacific oceans  
- SSS decrease despite the strong damping term
- in zonal mean -0.1 PSU over 300 meters beyond 50°N and S
- temperature strongly increase beyond 0.2 °C / PHC_37 at 100 meters everywhere but under sea-ice
where the wind module is set to zero in TKE
- SST patterns are cooler than in PHC37 in tropiacal and sub-polar gyres by -0.2°C whereas a small 
warming in the equatorial strip 
- in zonal mean -0.3°C off the Antarctic over 300 meters depth
- strong reduction over ~300 meters on the top part of the Deacon cell by -3 Sv 
- deeper MXL especially along the ACC path O(+50m)
- shallower MXL in main North deep water formation areas
- increase in tropical gyres of the Net surface heat fluxes / PHC_37 ~O(-3 w.m-2)  

Bilan (Sv) en moyenne annuelle pour l"experience:  PHC44
                                
           Precip  :       11.310391
 NOT modif Runoff  :       1.1496420
     modif Runoff  :       1.1240586
           ErP     :      -0.4116920
           EmPold  :       0.0000000
           -----------------------------
           EmP     :    -0.031959219

Evap a partir du flux Qla (pour information, non utilisee) : Evap_Svqla = 13.656075 Sv
Evap a partir des termes EmP, precip, ErP, runoff et EmPold: Evap_sv    = 12.814183 Sv

Bilan gain .vs. perte:
           Precip+Runoff_MOD :       12.434450 Sv
           Evap+ErP+EmPold   :       12.402491 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: