Variability and Uncertainty of Satellite Sea Surface Salinity in the Subpolar North Atlantic (2010–2019)

Satellite remote sensing of sea surface salinity (SSS) in the recent decade (2010–2019) has proven the capability of L-band (1.4 GHz) measurements to resolve SSS spatiotemporal variability in the tropical and subtropical oceans. However, the fidelity of SSS retrievals in cold waters at mid-high lati...

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Published in:Remote Sensing
Main Author: Lisan Yu
Format: Text
Language:English
Published: Multidisciplinary Digital Publishing Institute 2020
Subjects:
Online Access:https://doi.org/10.3390/rs12132092
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spelling ftmdpi:oai:mdpi.com:/2072-4292/12/13/2092/ 2023-08-20T04:04:46+02:00 Variability and Uncertainty of Satellite Sea Surface Salinity in the Subpolar North Atlantic (2010–2019) Lisan Yu agris 2020-06-30 application/pdf https://doi.org/10.3390/rs12132092 EN eng Multidisciplinary Digital Publishing Institute Ocean Remote Sensing https://dx.doi.org/10.3390/rs12132092 https://creativecommons.org/licenses/by/4.0/ Remote Sensing; Volume 12; Issue 13; Pages: 2092 sea surface salinity subpolar North Atlantic SMAP SMOS Argo harmonic analysis seasonal and interannual variations Text 2020 ftmdpi https://doi.org/10.3390/rs12132092 2023-07-31T23:42:37Z Satellite remote sensing of sea surface salinity (SSS) in the recent decade (2010–2019) has proven the capability of L-band (1.4 GHz) measurements to resolve SSS spatiotemporal variability in the tropical and subtropical oceans. However, the fidelity of SSS retrievals in cold waters at mid-high latitudes has yet to be established. Here, four SSS products derived from two satellite missions were evaluated in the subpolar North Atlantic Ocean in reference to two in situ gridded products. Harmonic analysis of annual and semiannual cycles in in situ products revealed that seasonal variations of SSS are dominated by an annual cycle, with a maximum in March and a minimum in September. The annual amplitudes are larger (>0.3 practical salinity scale (pss)) in the western basin where surface waters are colder and fresher, and weaker (~0.06 pss) in the eastern basin where surface waters are warmer and saltier. Satellite SSS products have difficulty producing the right annual cycle, particularly in the Labrador/Irminger seas where the SSS seasonality is dictated by the influx of Arctic low-salinity waters along the boundary currents. The study also found that there are basin-scale, time-varying drifts in the decade-long SMOS data records, which need to be corrected before the datasets can be used for studying climate variability of SSS. Text Arctic North Atlantic MDPI Open Access Publishing Arctic Western Basin Remote Sensing 12 13 2092
institution Open Polar
collection MDPI Open Access Publishing
op_collection_id ftmdpi
language English
topic sea surface salinity
subpolar North Atlantic
SMAP
SMOS
Argo
harmonic analysis
seasonal and interannual variations
spellingShingle sea surface salinity
subpolar North Atlantic
SMAP
SMOS
Argo
harmonic analysis
seasonal and interannual variations
Lisan Yu
Variability and Uncertainty of Satellite Sea Surface Salinity in the Subpolar North Atlantic (2010–2019)
topic_facet sea surface salinity
subpolar North Atlantic
SMAP
SMOS
Argo
harmonic analysis
seasonal and interannual variations
description Satellite remote sensing of sea surface salinity (SSS) in the recent decade (2010–2019) has proven the capability of L-band (1.4 GHz) measurements to resolve SSS spatiotemporal variability in the tropical and subtropical oceans. However, the fidelity of SSS retrievals in cold waters at mid-high latitudes has yet to be established. Here, four SSS products derived from two satellite missions were evaluated in the subpolar North Atlantic Ocean in reference to two in situ gridded products. Harmonic analysis of annual and semiannual cycles in in situ products revealed that seasonal variations of SSS are dominated by an annual cycle, with a maximum in March and a minimum in September. The annual amplitudes are larger (>0.3 practical salinity scale (pss)) in the western basin where surface waters are colder and fresher, and weaker (~0.06 pss) in the eastern basin where surface waters are warmer and saltier. Satellite SSS products have difficulty producing the right annual cycle, particularly in the Labrador/Irminger seas where the SSS seasonality is dictated by the influx of Arctic low-salinity waters along the boundary currents. The study also found that there are basin-scale, time-varying drifts in the decade-long SMOS data records, which need to be corrected before the datasets can be used for studying climate variability of SSS.
format Text
author Lisan Yu
author_facet Lisan Yu
author_sort Lisan Yu
title Variability and Uncertainty of Satellite Sea Surface Salinity in the Subpolar North Atlantic (2010–2019)
title_short Variability and Uncertainty of Satellite Sea Surface Salinity in the Subpolar North Atlantic (2010–2019)
title_full Variability and Uncertainty of Satellite Sea Surface Salinity in the Subpolar North Atlantic (2010–2019)
title_fullStr Variability and Uncertainty of Satellite Sea Surface Salinity in the Subpolar North Atlantic (2010–2019)
title_full_unstemmed Variability and Uncertainty of Satellite Sea Surface Salinity in the Subpolar North Atlantic (2010–2019)
title_sort variability and uncertainty of satellite sea surface salinity in the subpolar north atlantic (2010–2019)
publisher Multidisciplinary Digital Publishing Institute
publishDate 2020
url https://doi.org/10.3390/rs12132092
op_coverage agris
geographic Arctic
Western Basin
geographic_facet Arctic
Western Basin
genre Arctic
North Atlantic
genre_facet Arctic
North Atlantic
op_source Remote Sensing; Volume 12; Issue 13; Pages: 2092
op_relation Ocean Remote Sensing
https://dx.doi.org/10.3390/rs12132092
op_rights https://creativecommons.org/licenses/by/4.0/
op_doi https://doi.org/10.3390/rs12132092
container_title Remote Sensing
container_volume 12
container_issue 13
container_start_page 2092
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