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:

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DFS4 Air temperature correction applied:

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PHC32 corrected Air temperature & diff. with initial DFS4

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Time series

Year 100 | Temperature differences at z=105 m with Levitus and PHC_16:

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Year 100 | Salinity differences at z=105 m with Levitus and PHC_16:

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Year 100 | SSS differences with Levitus and PHC_16:

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Year 100 | Temperature differences in zonal average with Levitus and PHC_16:

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Year 100 | Salinity differences in zonal average with Levitus and PHC_16:

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Year 100 | Equatorial differences with Levitus and PHC_16 of zonal velocity U:

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Year 100 | Equatorial differences with Levitus and PHC_16 of temperature:

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Year 100 | Equatorial differences with Levitus and PHC_16 of salinity:

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Year 100 | Pacific equatorial differences with Levitus and PHC_16 of temperature:

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Year 100 | Qnet differences with PHC_16 :

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Year 100 | Global MOC:

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Year 100 | Atlantic MOC:

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Year 100 | BSF:

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Year 100 | Mediterranean water Lat: 40°N, depth 700 m:

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Year 100 | Mediterranean water Lat: 38°N, depth 1000 m:

Year 100 | Erp & Mxl fields:

Year 100 | Temperature & Salinity horizontal mean :

Year 100 | Straits transport: