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Changeset 2483 for branches/nemo_v3_3_beta/DOC/TexFiles/Chapters/Chap_OBS.tex – NEMO

Ignore:
Timestamp:
2010-12-18T13:36:55+01:00 (14 years ago)
Author:
djlea
Message:

Documentation fixes for OBS and ASM

File:
1 edited

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  • branches/nemo_v3_3_beta/DOC/TexFiles/Chapters/Chap_OBS.tex

    r2474 r2483  
    1414 
    1515The observation and model comparison code (OBS) reads in observation files 
    16 (profile temperature and salinity, sea surface temperature, sea level anomaly 
    17 and sea ice concentration) and calculates  an interpolated model equivalent 
     16(profile temperature and salinity, sea surface temperature, sea level anomaly, 
     17sea ice concentration, and velocity) and calculates  an interpolated model equivalent 
    1818value at the observation location and nearest model timestep. The OBS code is 
    1919called from \np{opa.F90} in order to initialise the model and to calculate the 
     
    2626For {\em in situ} profiles, a 1D vertical interpolator is needed in addition to 
    2727provide model fields at the observation depths. Currently this only works in 
    28 z-level model configurations but is currently being developed to work with a 
     28z-level model configurations, but is being developed to work with a 
    2929generalised vertical coordinate system. 
    30 Temperature data from moored buoys (TAO, TRITON, PIRATA) which in the 
     30Temperature data from moored buoys (TAO, TRITON, PIRATA) in the 
    3131ENACT/ENSEMBLES data-base are available as daily averaged quantities. For this 
    32 type of observations the 
     32type of observation the 
    3333observation operator will compare such observations to the model temperature 
    34 fields over one day. The relevant observation type may be specified in the namelist 
     34fields averaged over one day. The relevant observation type may be specified in the namelist 
    3535using \np{endailyavtypes}. Otherwise the model value from the nearest 
    3636timestep to the observation time is used. 
    3737 
    38 The resulting data is saved in a ``feedback'' file (or files) which can be used 
     38The resulting data are saved in a ``feedback'' file (or files) which can be used 
    3939for model validation and verification and also to provide information for data 
    4040assimilation. This code is controlled by the namelist \textit{nam\_obs}. To 
     
    643643  iterative scheme that involves first mapping a quadrilateral cell 
    644644  into a cell with coordinates (0,0), (1,0), (0,1) and (1,1). This 
    645   method is based on the SCRIP interpolation package \citep{Jones_MWR99,Jones_Bk01}. 
     645  method is based on the SCRIP interpolation package \citep{Jones_1998}. 
    646646   
    647647\end{enumerate} 
     
    702702P and B, etc.. The method used is 
    703703similar to the method used in 
    704 the Scripp interpolation package \citep{Jones_Bk01}. 
     704the SCRIP interpolation package \citep{Jones_1998}. 
    705705 
    706706In order to speed up the grid search, there is the possibility to construct  
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