Glorys2v4 reanalysis
WebIn a number of regions, the ensemble mean may even provide a more reliable estimate than any individual reanalysis product. Four reanalyses have been selected to contribute to … WebMay 26, 2024 · GLORYS2v4 is an ocean reanalysis, which is a scientific method that produces a comprehensive record of how ocean properties are changing over time. This reanalysis is performed with the NEMOv3.1 ocean model in configuration ORCA025_LIM. The vertical grid has 75 levels in depth with partial steps at the bottom.
Glorys2v4 reanalysis
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WebReference : GLORYS2V4 SYSTEM FOR GLOBAL OCEAN PHYSICAL REANALYSIS AT 1/4° Mercator Ocean - Latest update : May 2015 Geographical coverage : Global Ocean (180°W-180°E; 77°S-90°N) Physics or Biogeochemistry : Physics Grid and Resolutions : ORCA025 [1/4°; 75 levels] Grid size : 1442x1021x50 (partial steps) Code et Version : … WebDownload scientific diagram Schematics of the tropical Atlantic Ocean circulation system, overlaid onto the distribution of the 18°C isothermal depth in April 2010 from the GLORYS2v4 reanalysis.
WebHome - Mercator Océan - Ocean Forecasters WebThe reanalysis is built to be as close as possible to the observations (i.e. realistic) and in agreement with the model physics. It covers the period 1993 to 2015. ... GLORYS2V4 reanalysis relies on three main components: 1. the ocean model (including the surface atmospheric boundary condition) 2. the data assimilation method
WebAug 15, 2024 · MNG Laboratories (Medical Neurogenetics, LLC.), MNG; 5424 Glenridge Dr; Atlanta, Georgia, United States 30342; Phone: 678-225-0222 Fax: 678-225-0212 WebMay 25, 2024 · Reanalysis Model GLORYS2V4. The Mercator Ocean team computed and provided monthly-averaged values from the reanalysis model GLORYS2V4 (eddy-permitting with ≅ 0.25° resolution; CMEMS, 2024). The monthly climatology includes values of salinity, temperature, and the three-dimensional velocity field, as calculated using the …
WebSep 1, 2024 · The surface temperature fields obtained using different tracer OBC schemes were also compared to the GLORYS2V4 reanalysis. We used the RMSE metric with respect to the monthly-average reanalysis temperature fields. The results – for the same subdomain of Fig. 6 – are shown in Fig. 7. Download : Download high-res image (357KB)
WebApr 22, 2024 · The authors wish to acknowledge the Mercator Ocean for providing the GLORYS2v4 reanalysis data and the GTMBA Project Office of NOAA/PMEL for providing the PIRATA data. The authors are also thankful to our two anonymous reviewers for their constructive and useful comments and suggestions. This article is a publication of the … marlene musicWebThe reanalysis is run at eddy-permitting resolution (¼° horizontal resolution and 75 vertical levels) with the NEMO model and driven at the surface by ERA-Interim reanalysis from ECMWF (European Centre for Medium-Range Weather Forecasts). ... Performance and quality assessment of the global ocean eddy-permitting physical reanalysis … marlene nealWebReference : GLORYS2V4 SYSTEM FOR GLOBAL OCEAN PHYSICAL REANALYSIS AT 1/4° Mercator Ocean - Latest update : May 2015 Geographical coverage : Global Ocean … dartclipWebGLORYS2V4 hereafter), the latest ocean reanalysis produced at Mercator Ocean that covers the altime-try era (1993-2015) in the framework of Copernicus Marine … marlene name originThe Copernicus Marine Environment Monitoring Service (http://marine.copernicus.eu, hereafter referred to as Copernicus Marine Service or CMEMS) provides regular and systematic reference information on the physical state, variability and dynamics of the ocean, sea ice and marine ecosystems, for the global ocean and … See more The ingredients of the GLORYS12 reanalysis are largely those of the current real-time global CMEMS high-resolution forecasting system PSY4V3 (Lellouche et al., 2024). However, compared to the forecasting system, … See more This section gives a quality assessment of the different simulations, including comparisons with the assimilated observations as well … See more Three-dimensional average EKEs can also be assessed from GLORYS12, F12, and G4 daily velocity fields. Figure 12A shows the temporal evolution of the three-dimensional mean of monthly EKEs deduced from … See more dart clongriffinWebJul 23, 2024 · The first is the GLORYS2V4 global ocean reanalysis, which assimilates the observations from satellite altimetry, in situ profiles of temperature and salinity, sea surface temperature, and sea ice … marlene musicianWebvelocity) are: ORAS5, GloSea5, Glorys2v4, C-Glorsv7 and ECCO V4 R3. The first four all use 0.25o NEMO, but ECCO is very different (Fig 3 top) The AMOC strength is the sum of Ekman, Upper mid ocean and Florida current ... Reanalysis Ocean model Resolution Vertical coordinateSurface forcing What is assimilated and how? marlene napolitano