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Full text: The Copernicus marine service from 2015 to 2021

PUJOL, M.I'., FAUGERE, Y.', PASCUAL, A.?, DIBARBOURE, G., 
MORROW, RR.“ AND SL-TAC TEAM 
CLS, France, “IMEDEA, Spain, °CNES, France, *LEGOS, France 
1 
During the 6 years of Copernicus phase 1, the Sea Level 
Thematic Assembly Center (SL-TAC) has been completely 
transformed from a demonstration to a fully operational 
system. This transformation has been carried out according 
three main axes. 
First, the consolidation of the production robustness has 
been a major priority. Data from four new missions have 
been assimilated in 6 years: Jason-3, reference mission for 
climate scales (2016), Sentinel-3A (2017) and Sentinel-3B 
(since 2019) to complete coverage of mesocales. The 
Copernicus constellation is now operational and fully 
ingested in the SL-TAC system. To complete this coverage, 
the Chinese Collaborative mission HaiYang-2B was 
integrated in 2020, still increasing the sampling quality. 
From 4 missions in 2015, the near-real time (NRT) system 
Is now ingesting operationally 6 missions in 2021, ensuring 
the system robustness. The team has been reinforced and 
the DUACS software on which the SL-TAC production is 
based has been consolidated. Thanks to this efficient 
infrastructure, 22 new significant versions, impacting the 
product portfolio and content, were implemented. 
Then, the SL-TAC team worked on an extension and 
improvement of the product portfolio. The gridded products, 
highly popular among users, were added to the catalogue 
at the beginning of the project (2015), and several regional 
products were added after, such as the Europe (2019) 
aroduct and Mediterranean & Black Sea Mean Dynamic 
Topography (MDT) (2020). A whole set of variables is now 
available in products, such as absolute dynamic topography, 
geostrophic currents, and all the components needed by 
Monitoring Forecasting Centres (MFCs) to adapt the content 
of Sealevelto their model. The methodology of development 
in interaction with MFCs, initiated in the Tailored Altimeter 
Product for Assimilation Systems (TAPAS) group in 
MyOcean, has continued during the & years with annual 
meetings in order to achieve this evolution. This interaction 
detween producers and users was enabled by the 
copernicus Marine Service's (CMEMS) unique structure 
ncluding observations and models. Two full reprocessing 
were also implemented (2018, 2021) leading to major 
improvements. The precise multi-missions cross- 
calibration provided accurate Ocean Monitoring Indicator 
'OMI) such as the Global Mean Sea Level for climate 
application. The error budget of products has also been 
-efined and promoted through four peer-reviewed 
publications (Pujol et al., 2016, Taburet et al 2019, Ballarotta 
at al 2019, Sänchez-Romän et al., 2020) and Copernicus 
Marine Service Quality Information Documentation (QUID). 
Beside evolutions implemented within the Service the SL- 
"AC also has been preparing the next generation of 
products (with an enhanced special resolution) by 
integrating space Agencies (CNES, ESA) R&D. Demonstration 
samples, fully exploiting the altimetry content and with 
\mproved posting (1 km), have been proposed. Observation 
Simulation Experiment (OSE) tests carried out by MFCs 
showed a gain up to 10% in the model output assimilating 
these data (Benkiran et al., 2017). Similarly, the capacity of 
the high-resolution altimetry to improve the sampling of 
Sea level through “ice leads” was demonstrated. These 
studies allowed us to formulate recommendations to the 
Space Agencies concerning evolutions of upstream 
products. They also open very exciting prospects for the 
next phase of Copernicus Marine Service with new high- 
resolution product lines for nadir altimetry and the future 
Surface Water Ocean Topographv (SWOT) mission 
1. MAIN ACHIEVEMENTS FROM 2015 TO 
2021 
The SL-TAC has produced multi-mission altimetry Sea Leve 
products in NRT and Delayed Time (REP/DT) for MFCs and a 
various range of oceanographic applications for externa. 
users such as: climate forecastina centers, geophvsical and
	        
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