Mohid Ocean Downscalling - Revision history

Francisco: /* NOOA/GFS */

2017-05-23T13:36:47Z

‎NOOA/GFS

Francisco: /* MyOcean */

2017-05-23T13:34:00Z

‎MyOcean

Paulochambel: /* NOAA/GFS */

2015-10-26T18:08:20Z

‎NOAA/GFS

Paulochambel: /* NOAA/GFS */

2015-10-26T18:07:44Z

‎NOAA/GFS

Paulochambel: /* NOAA/GFS */

2015-10-26T18:05:45Z

‎NOAA/GFS

Paulochambel: /* NOAA/GFS */

2015-10-26T18:04:18Z

‎NOAA/GFS

Paulochambel: /* NOAA/GFS */

2015-10-26T18:00:24Z

‎NOAA/GFS

Paulochambel: /* Open boundary */

2013-05-30T13:10:52Z

‎Open boundary

Paulochambel: /* Open boundary */

2013-05-30T13:07:31Z

‎Open boundary

Paulochambel: /* Interpolation */

2013-05-30T13:04:45Z

‎Interpolation

@@ Line 5: / Line 5: @@
 ===NOOA/GFS===
-To download GFS model solution go to http://nomads.ncdc.noaa.gov/cgi-bin/ncdc-ui/define-collection.pl?model_sys=gfs4&model_name=gfs&grid_name=4. Then select date range(Ex.: 2013 April 15 To 2013 April 20), select cycles (Ex.: 0000), select forecast hours (Ex.: 003 006 009 012 015 018 021 024). Press Submit Data request button and Press Selected Files for FTP. On the Filename Filter Type “*.grb2” and press Select files button. Then select the levels desired and at FTP Information, type your email and press the start FTP button. This will place the files in the ftp for download.
+To download GFS model solution go to https://www.ncdc.noaa.gov/data-access/model-data/model-datasets/global-forcast-system-gfs. Then select your product of interest.
 ===CMEMS===

@@ Line 9: / Line 9: @@
 NOTES : This is a 24 hour period with all the necessary properties for Mohid, the best forecast for each day in the range. The 000 output is neglected because some properties are 3 hour average, for instance “downward solar radiation” isn’t present. For this 000 is subtracted and the 024 added.
-===MyOcean===
+===CMEMS===
-To download my ocean solution go to http://www.myocean.eu/. and click in ACCES THE CATALOGUE. In block 1 choose "Global Ocean", in 2 the parameters and in 3 choose forecast products. After fill all the blocks click search and in the next web page choose DATA ACCES and then GO. Prescribe the user name and password and then choose the dates and area of interest.
+The Copernicus Marine Environment Monitoring Service (CMEMS; http://marine.copernicus.eu/) is the follow up of the my ocean project. To download this solution access the catalogue http://marine.copernicus.eu/services-portfolio/access-to-products/ and select the GLOBAL_ANALYSIS_FORECAST_PHY_001_024. You will need to register in order to download your product of interest.
 ===RTOFS===

@@ Line 69: / Line 69: @@
 Running tool [[ConvertToHDF5|ConversionHDF5.exe]]
-Example of the file ConvertToHDF5.dat (for the keywords definition see [[ConvertToHDF5#CONVERT_GENERIC_NETCDF_CF | keyword definition for converting from netcdf CF to mohid hdf5]])
+Example of the file ConvertToHDF5.dat (see [[ConvertToHDF5#CONVERT_GENERIC_NETCDF_CF | keyword definition for converting from netcdf CF to mohid hdf5]])
   <begin_file>

@@ Line 69: / Line 69: @@
 Running tool [[ConvertToHDF5|ConversionHDF5.exe]]
-Example of the file ConvertToHDF5.dat (for the keywords definition see [[ConvertToHDF5#CONVERT_GENERIC_NETCDF_CF]])
+Example of the file ConvertToHDF5.dat (for the keywords definition see [[ConvertToHDF5#CONVERT_GENERIC_NETCDF_CF | keyword definition for converting from netcdf CF to mohid hdf5]])
   <begin_file>

@@ Line 69: / Line 69: @@
 Running tool [[ConvertToHDF5|ConversionHDF5.exe]]
-Example of the file ConvertToHDF5.dat (for the keywords definition see [[ConvertToHDF5|CONVERT_GENERIC_NETCDF_CF]])
+Example of the file ConvertToHDF5.dat (for the keywords definition see [[ConvertToHDF5#CONVERT_GENERIC_NETCDF_CF]])
   <begin_file>

@@ Line 414: / Line 414: @@
 ===Open boundary ===
-Open boundary conditions are imposed in [[Module Hydrodynamic|hydrodynamic]] module of MOHID. These differs from Level 1 to Level n of nested aplications. Level 1 is a 2D barotropic model usualy forced only with tide (no wind in atmosphere and InterfaceWaterAir module) with a slow connection. From Level 2 to Level n of nested domains the models are 3D baroclinic (e.g., include th density gradientes efects) and the Open Boundary Conditions (OBC) are resolved by imposing a Flow Relaxation Scheme (FRS) similar to the one presented by Marchesiello et al. (2001). The FRS is applied to temperature (T), salinity (S) and velocities (U, V) (Martinsen and Engedahl, 1987) being combined with a radiation scheme from Flather (1976) for the barotropic mode. The baroclinic component of the pressure gradients, the wind stress and atmospheric pressure are connected slowly.
+Open boundary conditions are imposed in [[Module Hydrodynamic|hydrodynamic]] module of MOHID. These differs from Level 1 to Level n of nested aplications. Level 1 is a 2D barotropic model usualy forced only with tide (no wind in atmosphere and InterfaceWaterAir module) with a slow connection. From Level 2 to Level n of nested domains the models are 3D baroclinic (e.g., include th density gradientes efects) and the Open Boundary Conditions (OBC) are resolved by imposing a Flow Relaxation Scheme (FRS) similar to the one presented by Marchesiello et al. (2001). The FRS is applied to temperature (T), salinity (S) and velocities (U, V) (Martinsen and Engedahl, 1987) being combined with a radiation scheme from Flather (1976) for the barotropic mode.
 ====Level 1====

@@ Line 264: / Line 264: @@
 == Interpolation ==
-Vertical discretization of RTOFS and MyOcean model solutions correspond to the depth of the center of the cell. Since MOHID [[Module Geometry | geometry]] must be provided in thickness the depths must be convertes to top of the faces cell and then to thickness layers. In order to avoid this the new method of interpolating grids allow to provide the depth of the center of the cells in ConvertToHDF5.dat instead to use a thickness calculated baing on the centers depth. Th both samples are provided bellow.
+Vertical discretization of RTOFS and MyOcean model solutions correspond to the depth of the center of the cell. Since MOHID [[Module Geometry | geometry]] must be provided in thickness the depths must be convertes to top of the faces cell and then to thickness layers. In order to avoid this the new method of interpolating grids allow to provide the depth of the center of the cells in ConvertToHDF5.dat instead to use a thickness calculated based on the centers depth. Th both samples are provided bellow.
 === GFS to MOHID ===