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MERCATOR French Ocean System: High-Resolution North Atlantic and Mediterranean Product (assimilation by optimal interpolation of altimetry data only) Entry ID: PSY2V1 |
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Summary
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Abstract:
Mercator has been providing weekly analysis and real-time nowcast (T0), and forecast (T0+7 days and T0 +14 days) bulletins of the three-dimensional ocean in the North Atlantic and Mediterranean Sea since January 8th 2003. This High-resolution bulletin (PSY2V1; 1/15 degree; one point computed every 5 to 7 km throughout the region of interest; eddy-resolving) covers the North Atlantic and Mediterranean basin. For more information see Mercator Configurations Summary at "http://www.mercator-ocean.fr/html/mod_actu/public/welcome_en.php3" Additional information about the Model: --------------------------------------------------- Mercator ocean system is based on the 8.1 version of the OPA z-coordinates code (Madec et al. 1998). OPA is an incompressible Navier-Stokes primitive- equation model using Boussinesq rigid-lid approximation that describes the temporal evolution of velocity, temperature and salinity in three dimensions. Mixed layer dynamic is ruled by TKE turbulent closure equations (1.5 closure scheme) (Blanke et al. 1993). The ocean model configuration used in this prototype (PSY2) is the high resolution (1/15 degrees) "Prototype Atlantique Mediterranee" (PAM) between 9 degrees N and 70 degrees N with 43 vertical levels with layer thicknesses from 6 meters at the surface to 200 meters at the bottom of the Mediterranean basin and 300 meters at the bottom of the Atlantic ocean. It includes a very simple thermodynamic ice model ('IF' ice model). The bathymetry is processed from the Smith and Sandwell (1997) data base and ETOPO5. Momentum and heat forcings are daily ECMWF forcing. Surface temperature is restored from Reynolds analyses (Reynolds & Smith, 1994), which include satellite and in-situ observations. Surface salinity is restored from climatology. The model is initialized using Reynaud (Reynaud et al. 1998) seasonal climatology. A relaxation to seasonal Medatlas (2002) climatology is also applied below 500 meters in the Gulf of Cadiz to represent Mediterranean Outflow Water. Assimilation Method: -------------------------- The data assimilation method (SAM; Systeme d'Assimilation Mercator) used is the reduced-order optimal interpolation (OI) scheme SOFA (Sub Optimal Filtering of Altimetry) (De Mey and Benkiran, 2002) coupled with the PALM software coupler (PALM group, 2000). The baroclinic component is corrected applying a lifting-lowering method similar to Cooper and Haines method (1996). Data assimilation is stopped along isobaths 500m towards the coast. Sea level anomaly (SLA) from Jason1/ERS2-Envisat/GFO is assimilated along track, once a week. The mean sea surface height (MSSH) used during the assimilation process is the one from Rio et al. (2003) diagnosed from in-situ observations in the Atlantic ocean. In the Mediterranean basin, MSSH is made out of several numerical simulations. Version 1 products assimilates altimetry data (SLA) only, while version 2 products assimilates altimetry and in situ data (SLA, Sea Surface Temperature (SST), Sea Surface Salinity (SSS) and In situ profiles). Mercator bulletins contain a range of parameters selected to depict ocean conditions and dynamics. These include: salinity, temperature, surface currents, zonal, meridian and vertical velocities, transport, sea surface height, mixed layer depth, barotropic height, baroclinic height. "Model: analysis and forecasting" 3D ocean products can be accessed on-line through Mercator Web Products (full domain and zonal animations, whole maps, zonal maps, sections and moorings graphs). For additional product information see "http://www.mercator-ocean.fr/html/produits/description/welcome_en.html". Mercator web products are designed for a wide audience (freely available), while numerical products are files for professional users and are available on a remote server. Please make an e-mail request to products@mercator-ocean.fr Archive bulletins are also available to identify longer-term patterns. Mercator web High-resolution North Atlantic and Mediterranean (PSY2V1, 1/15 degrees) products can be browsed on MERCATOR product web site: "http://bulletin.mercator-ocean.fr/html/welcome_en.jsp" In the Mersea strand1 european project context, Mercator makes available via an DODS/Opendap server its PSY2 high-resolution prototype products since 01/06/2003. Mercator also offers access to its products via the LAS implemented in the Mersea context. Fields provided for the Mersea inter-comparison exercise are daily mean best estimate fields as well as T0+7 forecast. Class1 (2D and 3D oceanic variables), 2 (sections and moorings), 3 diagnostics are provided on the Mercator-Mersea DODS/Opendap (password protected). For more information see "http://strand1.mersea.eu.org/html/strand1/datalinks.html" For more information about DODS/Opendap and Live Access Server (LAS), see Numerical products handbook "http://www.mercator-ocean.fr/html/produits/description/welcome_en.html" |
Related URL
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Link:
VIEW PROJECT HOME PAGE
Description: Mercator Ocean Main Webpage Link: VIEW PROJECT HOME PAGE Description: Mercator Ocean Web products. 3D modelled ocean: nowcasts and forecasts (medium resolution Atlantic 1/3 degree; high resolution North Atlantic and Mediterranean 1/15 degree; global low resolution 2 degree); and global observed ocean, data intercomparison and 3 D reconstitution of oceanic fields. Link: VIEW PROJECT HOME PAGE Description: Mersea Ocean modelling system homepage. Access to the Mercator real-time web image High-resolution North Atlantic and Mediterranean (1/15 degree) products (public access) and numerical products through LAS and DODS/Opendap (restricted access) Link: VIEW RELATED INFORMATION Description: Mercator Web products hanbook webpage (including the "Model: analysis and forecasting" products handbook and the "Observed ocean" products handbook). This handbook gives you the keys to understanding the 2,000 images you can see every week in the Mercator Web bulletin. The "observed ocean" system is based on altimetry and in situ data measurements. Additional information about Mercator configuration can also be found. |
Parent DIF
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This data set description is a member of a collection. The collection is described in MERCATOR |
Geographic Coverage
| N: 67.0 | S: -5.0 | E: 18.0 | W: -100.0 |
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Data Set Citation
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Dataset Originator/Creator:
Mercator Ocean
Dataset Title: High-resolution North Atlantic and Mediterranean (PSY2V1) Version: V1 (assimilates altimetry data only) Online Resource: http://www.mercator-ocean.fr/html/mod_actu/public/welcome_en.php3 |
Temporal Coverage
| Start Date: 2003-01-08 |
Location Keywords
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OCEAN
> ATLANTIC OCEAN
> NORTH ATLANTIC OCEAN
OCEAN > ATLANTIC OCEAN > NORTH ATLANTIC OCEAN > MEDITERRANEAN SEA |
Data Resolution
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Latitude Resolution:
1/15 degrees (5-7km)
Longitude Resolution: 1/15 degrees (5-7km) Vertical Resolution: 43 levels from surface to bottom (12-200m) Temporal Resolution: daily, weekly |
Science Keywords
| OCEANS >OCEAN CIRCULATION >DIFFUSION [Definition] |
| OCEANS >OCEAN CIRCULATION >OCEAN CURRENTS [Definition] |
| OCEANS >OCEAN CIRCULATION >OCEAN MIXED LAYER [Definition] |
| OCEANS >OCEAN HEAT BUDGET >HEAT FLUX [Definition] |
| OCEANS >OCEAN TEMPERATURE >OCEAN MIXED LAYER [Definition] |
| OCEANS >OCEAN TEMPERATURE >SEA SURFACE TEMPERATURE [Definition] |
| OCEANS >OCEAN TEMPERATURE >THERMOCLINE [Definition] |
| OCEANS >OCEAN TEMPERATURE >WATER TEMPERATURE [Definition] |
| OCEANS >OCEAN WINDS >WIND STRESS [Definition] |
| OCEANS >SALINITY/DENSITY >HALOCLINE [Definition] |
| OCEANS >SALINITY/DENSITY >PYCNOCLINE [Definition] |
| OCEANS >SALINITY/DENSITY >SALINITY [Definition] |
| OCEANS >SEA SURFACE TOPOGRAPHY >SEA SURFACE HEIGHT [Definition] |
ISO Topic Category
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ELEVATION
OCEANS |
Platform
| ERS-2 >European Remote Sensing Satellite-2 [Information] |
| GFO-1 >GEOSAT FOLLOW-ON-1 [Information] |
| JASON-1 [Information] |
| NOAA POES >NOAA Polar Orbiting Environmental Satellites [Information] |
| ENVISAT >Environmental Satellite [Information] |
Instrument
| ALTIMETERS [Information] |
| RADAR ALTIMETERS [Information] |
| CTD >Conductivity, Temperature, Depth [Information] |
| DRIFTING BUOYS [Information] |
| XBT >Expendable Bathythermographs [Information] |
| AVHRR >Advanced Very High Resolution Radiometer [Information] |
| POSEIDON-2 >JASON-1 RADAR ALTIMETER [Information] |
Project
| GODAE >Global Ocean Data Assimilation Experiment [Information] |
| MERSEA >Marine Environment and Security for the European Area [Information] |
| MERCATOR >MERCATOR OCEAN-Operational Oceanography [Information] |
Access Constraints
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Mercator web real time image products (GIF format) are designed for a wide audience (freely available, except zonal maps younger than 30 days need authorized access), while numerical products are files for professional users and are available on a remote server with authorized access. Please, you must justify your request to these products. E-mail request to products@mercator-ocean.fr or download the form |
Keywords
| model assimilation |
| altimetry data |
| sea surface temperature |
| in situ data |
| model intercomparison |
| operational oceanography |
Data Set Progress
| IN WORK |
Originating Center
Data Center
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MERCATOR OCEAN-Operational Oceanography, France
[Information]
Data Center URL: http://www.mercator-ocean.fr/
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Distribution
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Distribution_Media:
LAS, DODS/Opendap Access (restricted access), Image Browse (public access)
Distribution_Format: GIF, NetCDF, CF/COARDS |
Personnel
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VINCENT
TOUMAZOU Role: TECHNICAL CONTACT Email: vincent.toumazou at mercator-ocean.fr |
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MELANIE
F.
MEAUX Role: DIF AUTHOR Email: gsfc-gcmduso at mail.nasa.gov |
Publications/References
Blanke B., and P. Delecluse, 1993 Variability of the tropical Atlantic ocean
simulated by a general circulation model with two different mixed layer
physics. J. Phys. Oceanogr. 23. 1363-1388.
Cooper, M and K.Haines, 1996 Altimeter assimilation with water property
conservation, Journal of Geophysical research, 101, 1059-1077
De Mey, P., M. Benkiran, 2002 A multivariate reduced-order optimal
interpolation method and its application to the Mediterranean basin-scale
circulation. In : Ocean Forecasting, Conceptual basis and applications, N.
Pinardi and J.D. Woods, Eds., Springer-Verlag, Berlin Heidelberg New York,
472pp.
Drillet Y., R. Bourdalle-Badie and L. Siefridt, 2004 The Meddies in the
Mercator North Atlantic and Mediterranean Sea eddy resolving model, Journal of
Geophysical research, in press.
Guinehut, S., Larnicol, G., Le Traon, P.Y., 2002 Design of an array of
profiling floats in the North Atlantic from model simulations. Journal of
Marine Systems, 35, 1-9.
Guinehut, S., Le Traon, P.Y., Larnicol, G., Philipps, S., 2004 Combining Argo
and remote-sensing data to estimate the ocean three-dimensional temperature
fields - A first approach based on simulated observations. Journal of Marine
Systems, 46 (1-4), 85-98.
Lagarde, T., Piacentini, A. and Thual O., 2001 A new representation of
data-assimilation methods: The PALM flow-charting approach. Q. J. R. Meteorol.
Soc., 127, 571, 189-207.
Madec G., P. Delecluse, M. Imbard and C. Levy, 1998 OPA8.1, ocean general
circulation model reference manual, Notes du pole de modelisation IPSL, 11.
MEDAR/MEDATLAS Group, MEDAR/MEDATLAS 2002 database Cruise inventory, observed
and analysed data of temperature and bio-chemical parameters (4 CD-Roms).
PALM group, Towards the implementation of a PALM coupler, 2000 State of play on
the PALM project, CERFACS technical report.
Reynaud T., P. Legrand, H. Mercier and B. Barnier, 1998 A new analysis of
hydrographic data in the Atlantic and its application to an inverse modelling
study, International WOCE newsletter, 32, 29-31.
Reynolds R.W. and Smith. T., 1994 Improved global sea surface temperature
analysis using optimum interpolation, Journal of Climate, 929-948.
Rio, M.-H., and F. Hernandez, 2003b A Mean Dynamic Topography computed over the
world ocean from altimetry, in-situ measurements and a geoid model, Journal of
Geophysical Research.
simulated by a general circulation model with two different mixed layer
physics. J. Phys. Oceanogr. 23. 1363-1388.
Cooper, M and K.Haines, 1996 Altimeter assimilation with water property
conservation, Journal of Geophysical research, 101, 1059-1077
De Mey, P., M. Benkiran, 2002 A multivariate reduced-order optimal
interpolation method and its application to the Mediterranean basin-scale
circulation. In : Ocean Forecasting, Conceptual basis and applications, N.
Pinardi and J.D. Woods, Eds., Springer-Verlag, Berlin Heidelberg New York,
472pp.
Drillet Y., R. Bourdalle-Badie and L. Siefridt, 2004 The Meddies in the
Mercator North Atlantic and Mediterranean Sea eddy resolving model, Journal of
Geophysical research, in press.
Guinehut, S., Larnicol, G., Le Traon, P.Y., 2002 Design of an array of
profiling floats in the North Atlantic from model simulations. Journal of
Marine Systems, 35, 1-9.
Guinehut, S., Le Traon, P.Y., Larnicol, G., Philipps, S., 2004 Combining Argo
and remote-sensing data to estimate the ocean three-dimensional temperature
fields - A first approach based on simulated observations. Journal of Marine
Systems, 46 (1-4), 85-98.
Lagarde, T., Piacentini, A. and Thual O., 2001 A new representation of
data-assimilation methods: The PALM flow-charting approach. Q. J. R. Meteorol.
Soc., 127, 571, 189-207.
Madec G., P. Delecluse, M. Imbard and C. Levy, 1998 OPA8.1, ocean general
circulation model reference manual, Notes du pole de modelisation IPSL, 11.
MEDAR/MEDATLAS Group, MEDAR/MEDATLAS 2002 database Cruise inventory, observed
and analysed data of temperature and bio-chemical parameters (4 CD-Roms).
PALM group, Towards the implementation of a PALM coupler, 2000 State of play on
the PALM project, CERFACS technical report.
Reynaud T., P. Legrand, H. Mercier and B. Barnier, 1998 A new analysis of
hydrographic data in the Atlantic and its application to an inverse modelling
study, International WOCE newsletter, 32, 29-31.
Reynolds R.W. and Smith. T., 1994 Improved global sea surface temperature
analysis using optimum interpolation, Journal of Climate, 929-948.
Rio, M.-H., and F. Hernandez, 2003b A Mean Dynamic Topography computed over the
world ocean from altimetry, in-situ measurements and a geoid model, Journal of
Geophysical Research.
Creation and Review Dates
DIF Creation Date:
2004-12-28
Last DIF Revision Date:
2009-04-15
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