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ticket/1296 (diff) – NEMO

Changes between Version 4 and Version 5 of ticket/1296


Ignore:
Timestamp:
2014-05-16T10:02:16+02:00 (10 years ago)
Author:
timgraham
Comment:

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  • ticket/1296

    v4 v5  
    2323'''Subroutines:''' 
    2424 
    25  * Copy of dia_tsd_read or modify dia_tsd_read to allow it to be used with different files (after initial conditions have been read)[[BR]]- tra_rlx_init: [[BR]]    read the namelist, read the mask file, calculate restoration coefficient[[BR]]- tra_rlx:[[BR]]    Calculate the trend at each point = rlx_mask * resto * (zts_dta - tsb)  (where zts_dta is the climatological value, resto is the restoration coefficient) and add to total trend[[BR]]    The climatology that we are relaxing to should be on the original model grid. Given the long time scales of the climatology compared to variations in SSH it seems reasonable not worry about the slight changes in vertical grid spacing.[[BR]]- Link to trends diagnostics to output the trends? 
     25 * Copy of dia_tsd_read or modify dia_tsd_read to allow it to be used with different files (after initial conditions have been read) 
     26 * tra_rlx_init: [[BR]]    read the namelist, read the mask file (maybe separate subroutine), calculate restoration coefficient 
     27 * tra_rlx:[[BR]]    Calculate the trend at each point = rlx_mask * resto * (zts_dta - tsb)  (where zts_dta is the climatological value, resto is the restoration coefficient) and add to total trend[[BR]]    The climatology that we are relaxing to should be on the original model grid. Given the long time scales of the climatology compared to variations in SSH it seems reasonable not worry about the slight changes in vertical grid spacing. 
     28 * Link to trends diagnostics to output the trends? 
    2629 
    2730----