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

Changes between Version 5 and Version 6 of user/ctlod/ORCA2Runs/PHC9


Ignore:
Timestamp:
2008-10-23T16:11:33+02:00 (16 years ago)
Author:
ctlod
Comment:

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  • user/ctlod/ORCA2Runs/PHC9

    v5 v6  
    44= '''PHC_9 run''' =  
    55This run is based on the PHC_8 one except on the way the wind stress and module are managed.[[BR]] 
    6 Wind stress seems to be too low (in PHC_8) in high latitudes compared to what we have in using standard CLIO data[[BR]] 
    7 this component is capital for the water mass formation & penetration in these areas so it must be increased. 
     6Wind stress seems to be too low (in PHC_8) in high latitudes compared to what we have in using standard [[BR]] 
     7CLIO data this component is capital for the water mass formation & penetration in these areas so it must be increased. 
    88So we do the following test:[[BR]] 
    99- compute off-line the daily climatology of the fields (||U||.u)clim and (||U||.v)clim using 6hourly wind velocities.[[BR]] 
     
    1515 
    1616=== DFS4 wind module and wind stress === 
     17Plots below show the folllowing fields: 
     18{{{ 
     19   * (||wndm||.U)clim - ||wndm||clim.Uclim  
     20   * (||wndm||.V)clim - ||wndm||clim.Vclim 
     21}}} 
    1722[[Image(DFS4_Strong_Smooth_Uu_Uv_1y.png,  60%)]] 
     23 
    1824 
    1925=== '''SST''' differences with Reynolds and PHC_8: ===