- Timestamp:
- 2010-12-18T13:36:55+01:00 (14 years ago)
- File:
-
- 1 edited
Legend:
- Unmodified
- Added
- Removed
-
branches/nemo_v3_3_beta/DOC/TexFiles/Chapters/Chap_OBS.tex
r2474 r2483 14 14 15 15 The 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 equivalent16 (profile temperature and salinity, sea surface temperature, sea level anomaly, 17 sea ice concentration, and velocity) and calculates an interpolated model equivalent 18 18 value at the observation location and nearest model timestep. The OBS code is 19 19 called from \np{opa.F90} in order to initialise the model and to calculate the … … 26 26 For {\em in situ} profiles, a 1D vertical interpolator is needed in addition to 27 27 provide model fields at the observation depths. Currently this only works in 28 z-level model configurations but is currentlybeing developed to work with a28 z-level model configurations, but is being developed to work with a 29 29 generalised vertical coordinate system. 30 Temperature data from moored buoys (TAO, TRITON, PIRATA) whichin the30 Temperature data from moored buoys (TAO, TRITON, PIRATA) in the 31 31 ENACT/ENSEMBLES data-base are available as daily averaged quantities. For this 32 type of observation sthe32 type of observation the 33 33 observation operator will compare such observations to the model temperature 34 fields over one day. The relevant observation type may be specified in the namelist34 fields averaged over one day. The relevant observation type may be specified in the namelist 35 35 using \np{endailyavtypes}. Otherwise the model value from the nearest 36 36 timestep to the observation time is used. 37 37 38 The resulting data issaved in a ``feedback'' file (or files) which can be used38 The resulting data are saved in a ``feedback'' file (or files) which can be used 39 39 for model validation and verification and also to provide information for data 40 40 assimilation. This code is controlled by the namelist \textit{nam\_obs}. To … … 643 643 iterative scheme that involves first mapping a quadrilateral cell 644 644 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}. 646 646 647 647 \end{enumerate} … … 702 702 P and B, etc.. The method used is 703 703 similar to the method used in 704 the S cripp interpolation package \citep{Jones_Bk01}.704 the SCRIP interpolation package \citep{Jones_1998}. 705 705 706 706 In order to speed up the grid search, there is the possibility to construct
Note: See TracChangeset
for help on using the changeset viewer.