PHC_32 run

This run is based on the PHC_16 one except that:
We apply a correction on air temperature from south until 65°S which mimics
differences between DFS4 & CLIO data. See following zonal profile shown just below.
The DFS4 Air temperature is warmer than the CLIO one reaching almost 4° C differences in Antarctic area.
The correction applied yields a stronger air temperature which the one expected reaching values almost -9°C close to Antarctica.

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DFS4 - CLIO air temperautre mean seasonal differences:

DFS4 Air temperature correction applied:

PHC32 corrected Air temperature & diff. with initial DFS4

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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

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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:

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 :

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: