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Sea Surface Salinity Distribution in the Southern Ocean as Observed from SpaceLarge-scale spatial and temporal variabilities of sea surface salinity (SSS) in the Southern Ocean from 2011 to 2017 were studied using products derived from microwave sensors on board Aquarius, Soil Moisture and Ocean Salinity (SMOS), and Soil Moisture Active and Passive (SMAP) satellites. Four products, three from Aquarius and one from SMOS, were evaluated and shown to be generally consistent within 0.3 to 0.6 psu and agree favorably with in situ measurements. However, although the Aquarius products show consistent seasonality of SSS with high values of 34.45 psu in October and low values of 33.40 psu in May, theSMOS and SMAP products lack such seasonal variations. This may be caused by larger uncertainties in the SMOS and SMAP data due in part to the lack of concurrent scatterometer measurements that is used to correct for roughness effects. The four products provide similar spatial distributions of SSS with root mean square difference from 0.25 to 0.58 psu. Differences among Aquarius products are mainly due to varying salinity retrieval algorithms, smoothing, and masking of sea ice, while the SMOS product showed the highest SSS deviation that is likely due to the bias adjustment done on the data set. Our analyses show that SSS in the Southern Ocean region has significant meridional variations with the lowest SSS near the ice edge and highest at lower latitudes. The SSS is also lowest in summer indicating the predominant influence of sea ice and glacial melt, but it stays low near ice edges even during the growth season. Salinity together with temperature is the key parameters that control the state and circulation of the World's oceans. The large‐scale distribution of the sea surface salinity of the Southern Ocean is quantified for the first time using Aquarius, Soil Moisture and Ocean Salinity, and Soil
Moisture Active and Passive satellite microwave data. Seasonal and interannual changes in the distribution
as affected by the sea ice cover, surface temperature, and precipitation are evaluated. Comparative studies
were done, using four different products that are publicly available, in conjunction with in situ observations
to gain insights into the true nature of the distribution and how consistently the sea surface salinity is
depicted by the different products. There are general consistencies in the products, and discrepancies are
attributed to different algorithms, smoothing techniques, and sea ice masking. Aquarius data are shown to
have higher accuracy than Soil Moisture and Ocean Salinity and Soil Moisture Active and Passive products
in part because of having concurrent scatterometer that provides accurate correction to roughness effects.






Document ID
20190030481
Acquisition Source
Goddard Space Flight Center
Document Type
Reprint (Version printed in journal)
External Source(s)
Authors
Garcia-Eidell, Cynthia
(Illinois Univ. Chicago, IL, United States)
Comiso, Josefino C.
(Illinois Univ. Chicago, IL, United States)
Dinnat, Emmanuel
(Chapman Univ. Orange, CA, United States)
Brucker, Ludovic
(Universities Space Research Association (USRA) Moffett Field, CA, United States)
Date Acquired
September 5, 2019
Publication Date
May 22, 2019
Publication Information
Publication: Journal of Geophysical Research (JGR) Oceans
Publisher: American Geophysical Union (AGU)
Volume: 124
Issue: 5
ISSN: 2169-9291
e-ISSN: 2169-9275
Subject Category
Geosciences (General)
Report/Patent Number
GSFC-E-DAA-TN72859
ISSN: 2169-9291
Report Number: GSFC-E-DAA-TN72859
E-ISSN: 2169-9275
Funding Number(s)
CONTRACT_GRANT: 80NSSC18K1443
CONTRACT_GRANT: NNG11HP16A
Distribution Limits
Public
Copyright
Other

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