FN Archimer Export Format PT J TI Assessing the impact of multiple altimeter missions and Argo in a global eddy-permitting data assimilation system BT AF VERRIER, Simon LE TRAON, Pierre-Yves REMY, Elisabeth AS 1:1,2;2:1,2;3:1; FF 1:PDG-ODE-LOPS-SIAM;2:PDG-ODE-ADM3;3:; C1 Mercator Ocean, F-31520 Ramonville St Agne, France. IFREMER, F-29280 Plouzane, France. C2 MERCATOR OCEAN, FRANCE IFREMER, FRANCE SI BREST SE PDG-ODE-LOPS-SIAM PDG-ODE-ADM3 UM LOPS IN WOS Ifremer jusqu'en 2018 DOAJ copubli-france IF 2.289 TC 12 UR https://archimer.ifremer.fr/doc/00416/52780/53660.pdf LA English DT Article AB A series of observing system simulation experiments (OSSEs) is carried out with a global data assimilation system at 1∕4° resolution using simulated data derived from a 1∕12° resolution free-run simulation. The objective is to not only quantify how well multiple altimeter missions and Argo profiling floats can constrain the global ocean analysis and 7-day forecast at 1∕4° resolution but also to better understand the sensitivity of results to data assimilation techniques used in Mercator Ocean operational systems. The impact of multiple altimeter data is clearly evidenced even at a 1∕4° resolution. Seven-day forecasts of sea level and ocean currents are significantly improved when moving from one altimeter to two altimeters not only on the sea level, but also on the 3-D thermohaline structure and currents. In high-eddy-energy regions, sea level and surface current 7-day forecast errors when assimilating one altimeter data set are respectively 20 and 45 % of the error of the simulation without assimilation. Seven-day forecasts of sea level and ocean currents continue to be improved when moving from one altimeter to two altimeters with a relative error reduction of almost 30 %. The addition of a third altimeter still improves the 7-day forecasts even at this medium 1∕4° resolution and brings an additional relative error reduction of about 10 %. The error level of the analysis with one altimeter is close to the 7-day forecast error level when two or three altimeter data sets are assimilated. Assimilating altimeter data also improves the representation of the 3-D ocean fields. The addition of Argo has a major impact on improving temperature and demonstrates the essential role of Argo together with altimetry in constraining a global data assimilation system. Salinity fields are only marginally improved. Results derived from these OSSEs are consistent with those derived from experiments with real data (observing system evaluations, OSEs) but they allow for more detailed characterisation of errors on analyses and 7-day forecasts. Both OSEs and OSSEs should be systematically used and intercompared to test data assimilation systems and quantify the impact of existing observing systems. PY 2017 PD DEC SO Ocean Science SN 1812-0784 PU Copernicus Gesellschaft Mbh VL 13 IS 6 UT 000418199300002 BP 1077 EP 1092 DI 10.5194/os-13-1077-2017 ID 52780 ER EF