2021
DOI: 10.1002/essoar.10507337.1
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Satellite-based Time-Series of Sea Surface Salinity designed for Ocean and Climate Studies

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Cited by 2 publications
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“…These data are only available since 2002 and were therefore only used to study the variability of SST within the period of the cruise; (III) Surface chlorophyll-a concentration L4 (gridded and gap-filled) product from Marine Copernicus (CMEMS) with 4 km resolution (Garnesson et al, 2019) within the period of the cruise; (IV) L4 Sea Surface Salinity (SSS) v03.21 from the European Space Agency Sea Surface Salinity Climate Change Initiative consortium at 50 km and a weekly resolution, spatially sampled on a 25 km EASE (Equal-Area Scalable Earth) grid and 1 day of time sampling. This dataset combines the satellite measurements from SMOS, SMAP, and Aquarius covering the period January 2010-September 2020 (see Boutin et al, 2021); (V) Ssalto/Duacs Multimission Altimeter derived absolute dynamic topography (ADT) and derived surface geostrophic velocity fields at a 0.25 • horizontal grid for the period 1993-2019 distributed by CMEMS (Capet et al, 2014;Pujol et al, 2016). This latter dataset is also used as input for the Tracked Ocean Eddies (TOEddies) automatic detection algorithm developed by Chaigneau et al (2011), Pegliasco et al (2015 and Laxenaire et al (2018Laxenaire et al ( , 2019Laxenaire et al ( , 2020.…”
Section: Datamentioning
confidence: 99%
“…These data are only available since 2002 and were therefore only used to study the variability of SST within the period of the cruise; (III) Surface chlorophyll-a concentration L4 (gridded and gap-filled) product from Marine Copernicus (CMEMS) with 4 km resolution (Garnesson et al, 2019) within the period of the cruise; (IV) L4 Sea Surface Salinity (SSS) v03.21 from the European Space Agency Sea Surface Salinity Climate Change Initiative consortium at 50 km and a weekly resolution, spatially sampled on a 25 km EASE (Equal-Area Scalable Earth) grid and 1 day of time sampling. This dataset combines the satellite measurements from SMOS, SMAP, and Aquarius covering the period January 2010-September 2020 (see Boutin et al, 2021); (V) Ssalto/Duacs Multimission Altimeter derived absolute dynamic topography (ADT) and derived surface geostrophic velocity fields at a 0.25 • horizontal grid for the period 1993-2019 distributed by CMEMS (Capet et al, 2014;Pujol et al, 2016). This latter dataset is also used as input for the Tracked Ocean Eddies (TOEddies) automatic detection algorithm developed by Chaigneau et al (2011), Pegliasco et al (2015 and Laxenaire et al (2018Laxenaire et al ( , 2019Laxenaire et al ( , 2020.…”
Section: Datamentioning
confidence: 99%