PHC_34 run

This run is based on the PHC_16 one except that: nn_sssr = 2 instead 1 as in PHC_16, i.e. we take into account modification of volume flux in the emp term.
Few patterns list:

- +0.2 PSU in Artcic area at ~100 meters deep

# 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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# 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: