Sea surface salinity variability from satellite and in situ observations around Greenland
Reverdin, G.; Bonjean, F.; Kilian, L.; Boutin, J.; Guimbard, S.; Vergely, J.-L.; Foukal, N.; de Jong, M.F.; Duyck, E.; Stedmon, C.A.; Khvorostyanov, D. (2025). Sea surface salinity variability from satellite and in situ observations around Greenland. J. Atmos. Oceanic. Technol. 42(10): 1247-1261. https://dx.doi.org/10.1175/jtech-d-24-0105.1
In: Journal of Atmospheric and Oceanic Technology. American Meteorological Society: Boston, MA. ISSN 0739-0572; e-ISSN 1520-0426, more
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| Author keywords |
Band-L radiometry; SSS; North Atlantic subpolar gyre; Labrador Sea; Greenland shelves |
| Authors | | Top |
- Reverdin, G.
- Bonjean, F.
- Kilian, L.
- Boutin, J.
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- Guimbard, S.
- Vergely, J.-L.
- Foukal, N.
- de Jong, M.F., more
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- Duyck, E., more
- Stedmon, C.A.
- Khvorostyanov, D.
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| Abstract |
This study investigates sea surface salinity (SSS) south of Greenland using satellite radiometric data products at pixel resolution and quality-assured in situ measurements. The analysis focuses on the weekly Climate Change Initiative (CCI), version 4.4, dataset from the European Space Agency (ESA), covering 2010–22, and the high-temporal-resolution dataset from the Downstream Data Processing Center for Soil Moisture Ocean Salinity (SMOS)—High Resolution (CATDS-HR), available for 2015–22. Both satellite data products reveal significant positive biases on the shelves, with the CCI, version 4.4, product removing more data in this region and underestimating variability by at least a factor of 2 compared to CATDS-HR. In regions with low SSS variability, such as the central North Atlantic subpolar gyre, satellite products overestimate variability by 40% [0.17 instead of 0.12 on the Practical Salinity Scale (pss)] due to retrieval uncertainties (∼0.14 pss). However, CATDS-HR is 10% closer to in situ measurements than CCI, version 4. Beyond 100 km from the Greenland coast, in areas of high SSS variability, both products capture significant seasonal and interannual patterns, resolving scales down to 50 km. Satellite and in situ data for 2010–22 highlight an extreme freshwater event in the eastern Labrador Sea in September–October 2021, characterized by a > 2 pss salinity decrease near the Greenland continental slope that diminishes to > 1 pss up to 300 km offshore. These results demonstrate the capability of satellite SSS products to resolve freshwater exchange from Greenland shelves to the ocean interior, while emphasizing the need for adjustments to address systematic biases closer to the coast. |
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