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user/ctlod/ORCA2Runs/PHC9 (diff) – NEMO

Changes between Version 3 and Version 4 of user/ctlod/ORCA2Runs/PHC9


Ignore:
Timestamp:
2008-10-22T18:35:35+02:00 (15 years ago)
Author:
ctlod
Comment:

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  • user/ctlod/ORCA2Runs/PHC9

    v3 v4  
    66Wind stress seems to be too low (in PHC_8) in high latitudes compared to what we have in using standard CLIO data[[BR]] 
    77this component is capital for the water mass formation & penetration in these areas so it must be increased. 
    8  
    9 To do so, we do the following test:[[BR]] 
    10 - compute off-line the daily climatology of the components ||U||.u and ||U||.v using 6hourly wind velocities.[[BR]] 
     8So we do the following test:[[BR]] 
     9- compute off-line the daily climatology of the fields (||U||.u)clim and (||U||.v)clim using 6hourly wind velocities.[[BR]] 
    1110- we use the wind module computed with the 6hourly wind velocities which is much more energetics than the one computed using climatological velocities.[[BR]] 
    1211 
    13 Note that we don't substract the ocean/sea-ice velocities when computing the wind module since it is no more possible. 
     12Note that we don't substract the ocean/sea-ice velocities when computing the wind module since this last is now read. 
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     14---- 
    2115 
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