Version 15 (modified by ctlod, 12 years ago) (diff)


PHC_16 run

This run is based on the PHC_15 one except that the precipitation & runoff have been reduce by 9% instead of 8% in PHC_15.
The idea here is to minimize the SSH drift and the Empold values. The result is positive.

Comparisons (when done) are done relatively to the PHC_10 experiment to emphaze the impact of using the Kz tides parameterization especially on the ITF area.

Runs PHC_10 PHC_11 PHC_15 PHC_16
Precip -8% -8% -8% -9%
Evap +10% +10% +10% +10%
Empold (Sv) +0.1 +0.12 +0.13 -0.02
SST/rt PHC3 ?? ?? ?? ??
SSH drift (m) +0.008 +0.01 +0.01 -0.002

SST differences with Reynolds and PHC_10:


Temperature differences at z=105 m with Levitus and PHC_10:


SSS differences with Levitus and PHC_10:


Temperature differences in zonal average with Levitus and PHC_10:


Salinity differences in zonal average with Levitus and PHC_10:


Equatorial differences with Levitus and PHC_10 of zonal velocity U:


Equatorial differences with Levitus and PHC_10 of temperature:


Equatorial differences with Levitus and PHC_10 of salinity:


Pacific equatorial differences with Levitus and PHC_10 of temperature:


Qnet differences with PHC_10 :


Global MOC:


Atlantic MOC:


BSF:


Mediterranean water Lat: 40°N, depth 700 m:


Mediterranean water Lat: 38°N, depth 1000 m:

Erp & Mxl fields:

Straits transport:

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