FN Archimer Export Format PT J TI Assessing the Impact of the Assimilation of SWOT Observations in a Global High-Resolution Analysis and Forecasting System Part 1: Methods BT AF Benkiran, Mounir Ruggiero, Giovanni Greiner, Eric LE TRAON, Pierre-Yves Remy, Elisabeth Lellouche, Jean-Michel Bourdallé-Badie, Romain Drillet, Yann Tchonang, Babette AS 1:1;2:1;3:2;4:1,3;5:1;6:1;7:1;8:1;9:1; FF 1:;2:;3:;4:PDG-ODE;5:;6:;7:;8:;9:; C1 Mercator Ocean International, Ramonville-Saint-Agne, France Collecte Localisation Satellites, Ramonville-Saint-Agne, France Laboratoire Géodynamique et Enregistrements Sédimentaires, Institut Français de Recherche pour l’Exploitation de la Mer, Plouzané, France C2 MERCATOR OCEAN, FRANCE CLS, FRANCE IFREMER, FRANCE SI MERCATOR SE PDG-ODE IN WOS Ifremer UPR DOAJ copubli-france IF 5.247 TC 9 UR https://archimer.ifremer.fr/doc/00706/81787/86521.pdf https://archimer.ifremer.fr/doc/00706/81787/86522.jpeg LA English DT Article DE ;data assimilation;satellite altimetry;OSSE (Observing System Simulation Experiment);SWOT (Surface Water Ocean Topography);forecasting system AB The future Surface Water Ocean Topography (SWOT) mission due to be launched in 2022 will extend the capability of existing nadir altimeters to enable two-dimensional mapping at a much higher effective resolution. A significant challenge will be to assimilate this kind of data in high-resolution models. In this context, Observing System Simulation Experiments (OSSEs) have been performed to assess the impact of SWOT on the Mercator Ocean and Copernicus Marine Environment Monitoring Service (CMEMS) global, high-resolution analysis and forecasting system. This paper focusses on the design of these OSSEs, in terms of simulated observations and assimilation systems (ocean model and data assimilation schemes). The main results are discussed in a companion paper. Two main updates of the current Mercator Ocean data assimilation scheme have been made to improve the assimilation of information from SWOT data. The first one is related to a different parametrisation of the model error covariance, and the second to the use of a four-dimensional (4D) version of the data assimilation scheme. These improvements are described in detail and their contribution is quantified. The Nature Run (NR) used to represent the “truth ocean” is validated by comparing it with altimeter observations, and is then used to simulate pseudo-observations required for the OSSEs. Finally, the design of the OSSEs is evaluated by ensuring that the differences between the assimilation system and the NR are statistically consistent with the misfits between real ocean observations and real-time operational systems. PY 2021 PD JUN SO Frontiers In Marine Science SN 2296-7745 PU Frontiers Media VL 8 UT 000689507300001 DI 10.3389/fmars.2021.691955 ID 81787 ER EF