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:

# 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 : -2.6312896 ErP_new : -2.5409565 EmPold? : 0.77961481 ----------------------------- EmP : 0.033778881

Evap a partir du flux Qla (pour information, non utilisee) : Evap_Svqla = 13.742580 Sv Evap a partir des termes EmP, precip, ErP, runoff et EmPold?: Evap_sv = 14.319903 Sv

Bilan gain .vs. perte:

Precip+Runoff_MOD : 12.434450 Sv Evap+ErP+EmPold? : 12.468229 Sv

# 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

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# Seasonal mean for the year 101

Antarctic MXL

Antarctic Sea-ice Thickness

Arctic MXL

Arctic Sea-ice Thickness

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# Year 100

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

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: