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<a name="introduction-contents"></a>
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<a name="introduction-contents"></a>
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===============================
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===============================
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## Contents
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## Contents
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-----
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<a name="introduction-contents-models-version"></a>
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<a name="introduction-contents-models-version"></a>
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========================
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========================
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* _WRF_ is a LAM (limited area model) developed by the NCAR, the atmospheric research american center. The Weather Research and Forecasting (WRF) Model is a next-generation mesoscale numerical weather prediction system designed to serve both atmospheric research and operational forecasting needs.
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* _WRF_ is a LAM (limited area model) developed by the NCAR, the atmospheric research american center. The Weather Research and Forecasting (WRF) Model is a next-generation mesoscale numerical weather prediction system designed to serve both atmospheric research and operational forecasting needs.
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------
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------
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<a name="introduction-contents-listing-of-global-inputs-stored"></a>
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<a name="introduction-contents-listing-of-global-inputs-stored"></a>
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========================
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#### Listing of global inputs stored
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#### Listing of global inputs stored
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*OCEAN*
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**OCEAN** :
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MERCATOR GLORYS (GLobal Ocean ReanalYsis and Simulation) reanalysis are based on the PSY4 system which is a global high resolution ocean monitoring and forecasting system from Mercator.
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MERCATOR GLORYS (GLobal Ocean ReanalYsis and Simulation) reanalysis are based on the PSY4 system which is a global high resolution ocean monitoring and forecasting system from Mercator.
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* MERCATOR GLORYS2V4
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* MERCATOR GLORYS2V4
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> **Note** : CMEMS is the Copernicus Marine Environment Monitoring Service , which provide regular data from Mercator native data
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> **Note** : CMEMS is the Copernicus Marine Environment Monitoring Service , which provide regular data from Mercator native data
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---
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*ATMO*
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**ATMO** :
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* ERA5 reanalysis ECMWF 1h
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* ERA5 reanalysis ECMWF 1h
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It includes the following surface variables required by the NEMO bulk formula to calculate heat, freshwater and momentum fluxes across the air-sea interface (i.e. the surface boundary condition to the model primitive equations):
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It includes the following surface variables required by the NEMO bulk formula to calculate heat, freshwater and momentum fluxes across the air-sea interface (i.e. the surface boundary condition to the model primitive equations):
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✓ zonal and meridional components of the 10-m wind : u10, v10
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* zonal and meridional components of the 10-m wind : u10, v10
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✓ 2-m air humidity : q2
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* 2-m air humidity : q2
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✓ 2-m air temperature : t2
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* 2-m air temperature : t2
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✓ downward shortwave radiation at the sea surface : radsw
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* downward shortwave radiation at the sea surface : radsw
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✓ downward longwave radiation at thesea surface: radlw
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* downward longwave radiation at thesea surface: radlw
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✓ precipitation total and solid: P, snow
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* precipitation total and solid: P, snow
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✓ sea level pressure : slp (for DFS5.2 : 3h or from ERAinterim 6h)
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* sea level pressure : slp (for DFS5.2 : 3h or from ERAinterim 6h)
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*_The Making Of the DRAKKAR FORCING SET DFS5 from (https://www.drakkar-ocean.eu/publications/reports/report_DFS5v3_April2016.pdf)_
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*_The Making Of the DRAKKAR FORCING SET DFS5 from (https://www.drakkar-ocean.eu/publications/reports/report_DFS5v3_April2016.pdf)_
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> **Note** : CDS is the Climate Data Store , provide regular data from ECMWF native data
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> **Note** : CDS is the Climate Data Store , provide regular data from ECMWF native data
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*RUNOFF*
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**RUNOFF** :
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* ISBA-CTRIP land surface model daily runoff data from 1993 to 2017 (0.5°) ([B.Decharme](https://agupubs.onlinelibrary.wiley.com/doi/full/10.1029/2018MS001545))
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* ISBA-CTRIP land surface model daily runoff data from 1993 to 2017 (0.5°) ([B.Decharme](https://agupubs.onlinelibrary.wiley.com/doi/full/10.1029/2018MS001545))
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* [GLOFAS ERA5v2.1](images/howto_glofas_era5.png) : Operational global river discharge reanalysis was produced using the ERA5 ECMWF reanalysis / daily runoff data from 1979 to 2020 (0.1°)
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* [GLOFAS ERA5v2.1](images/howto_glofas_era5.png) : Operational global river discharge reanalysis was produced using the ERA5 ECMWF reanalysis / daily runoff data from 1979 to 2020 (0.1°)
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---
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*BATHY*
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**BATHY** :
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* Global Bathymetry from ETOPO1, ETOPO2
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* Global Bathymetry from ETOPO1, ETOPO2
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* Global Bathymetry from GEBCO 2019
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* Global Bathymetry from GEBCO 2019
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Is one of the first step of the preprocessing of a Nemo configuration. The interpolation onto the model grid has been conducted by taking all the original grid points falling into an NEMO grid box, and taking the median of those points.It s possible to choose the mean operator also. This procedure produces a smoothing of the sub-grid scale topography.
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Is one of the first step of the preprocessing of a Nemo configuration. The interpolation onto the model grid has been conducted by taking all the original grid points falling into an NEMO grid box, and taking the median of those points.It s possible to choose the mean operator also. This procedure produces a smoothing of the sub-grid scale topography.
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------
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------
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<a name="introduction-contents-repository-description"></a>
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<a name="introduction-contents-repository-description"></a>
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========================
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