Enhanced SMOS Sea Surface Salinity in the Western Mediterranean Sea: accuracy and mesoscale structures description

European Geosciences Union (EGU) General Assembly 2018, 8-13 April 2018, Vienna, Austria.-- 1 page The Mediterranean Sea is a hot spot for climate change. The water balance in the basin is characterized by anexcess of evaporation over precipitation and river runoff, which is compensated by the entra...

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Main Authors: Olmedo, Estrella, Alvera-Azcárate, Aida, Turiel, Antonio, Taupier-Letage, I.
Format: Conference Object
Language:unknown
Published: European Geosciences Union 2018
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Online Access:http://hdl.handle.net/10261/185268
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spelling ftcsic:oai:digital.csic.es:10261/185268 2024-02-11T10:06:37+01:00 Enhanced SMOS Sea Surface Salinity in the Western Mediterranean Sea: accuracy and mesoscale structures description Olmedo, Estrella Alvera-Azcárate, Aida Turiel, Antonio Taupier-Letage, I. 2018-04-08 http://hdl.handle.net/10261/185268 unknown European Geosciences Union Publisher's version https://meetingorganizer.copernicus.org/EGU2018/orals/26767 Sí issn: 1607-7962 Geophysical Research Abstracts 20: EGU2018-7919 (2018) http://hdl.handle.net/10261/185268 open comunicación de congreso http://purl.org/coar/resource_type/c_5794 2018 ftcsic 2024-01-16T10:40:57Z European Geosciences Union (EGU) General Assembly 2018, 8-13 April 2018, Vienna, Austria.-- 1 page The Mediterranean Sea is a hot spot for climate change. The water balance in the basin is characterized by anexcess of evaporation over precipitation and river runoff, which is compensated by the entrance of fresher waterfrom the Atlantic. This Atlantic water, AW, which spreads through the Mediterranean Sea, determines the surfacecirculation.In the Algerian Basin, AW forms an unstable current that generates fresh-core coastal eddies that propa-gate downstream, eventually offshore. The eddy activity in the region enhances the mixing of the recently enteredAW with the saltier resident water, strongly affecting the spatial distribution of salinity and, therefore, playinga major role in the surface circulation of the Mediterranean Sea. Besides, during winter, in the North WesternMediterranean, deep water convection occurs under the influence of dry and cold northerly winds.In such a context, data from Soil Moisture and Ocean Salinity (SMOS) European Space Agency (ESA)’smission spanning more than 8 years can help to gain a better understanding of the Sea Surface Salinity (SSS)dynamics in the Mediterranean Sea. Unfortunately, this critical area is strongly affected by Radio FrequencyInterference and systematic biases due to the coast contamination (also called Land-Sea contamination). Botheffects impair SMOS SSS retrieval in these areas.A new methodology using a combination of debiased non-Bayesian retrieval, DINEOF (Data InterpolatingEmpirical Orthogonal Functions) and multifractal fusion has been used to improve to improve SMOS SSS fieldsover the North Atlantic Ocean and the Mediterranean Sea. The debiased non-Bayesian retrieval mitigates thesystematic errors produced by the Land-Sea contamination. Besides, this retrieval improves the coverage bymeans of multiyear statistical filtering criteria. This methodology allows obtaining SMOS SSS fields in theMediterranean Sea. However, the resulting SSS suffers from a ... Conference Object North Atlantic Digital.CSIC (Spanish National Research Council)
institution Open Polar
collection Digital.CSIC (Spanish National Research Council)
op_collection_id ftcsic
language unknown
description European Geosciences Union (EGU) General Assembly 2018, 8-13 April 2018, Vienna, Austria.-- 1 page The Mediterranean Sea is a hot spot for climate change. The water balance in the basin is characterized by anexcess of evaporation over precipitation and river runoff, which is compensated by the entrance of fresher waterfrom the Atlantic. This Atlantic water, AW, which spreads through the Mediterranean Sea, determines the surfacecirculation.In the Algerian Basin, AW forms an unstable current that generates fresh-core coastal eddies that propa-gate downstream, eventually offshore. The eddy activity in the region enhances the mixing of the recently enteredAW with the saltier resident water, strongly affecting the spatial distribution of salinity and, therefore, playinga major role in the surface circulation of the Mediterranean Sea. Besides, during winter, in the North WesternMediterranean, deep water convection occurs under the influence of dry and cold northerly winds.In such a context, data from Soil Moisture and Ocean Salinity (SMOS) European Space Agency (ESA)’smission spanning more than 8 years can help to gain a better understanding of the Sea Surface Salinity (SSS)dynamics in the Mediterranean Sea. Unfortunately, this critical area is strongly affected by Radio FrequencyInterference and systematic biases due to the coast contamination (also called Land-Sea contamination). Botheffects impair SMOS SSS retrieval in these areas.A new methodology using a combination of debiased non-Bayesian retrieval, DINEOF (Data InterpolatingEmpirical Orthogonal Functions) and multifractal fusion has been used to improve to improve SMOS SSS fieldsover the North Atlantic Ocean and the Mediterranean Sea. The debiased non-Bayesian retrieval mitigates thesystematic errors produced by the Land-Sea contamination. Besides, this retrieval improves the coverage bymeans of multiyear statistical filtering criteria. This methodology allows obtaining SMOS SSS fields in theMediterranean Sea. However, the resulting SSS suffers from a ...
format Conference Object
author Olmedo, Estrella
Alvera-Azcárate, Aida
Turiel, Antonio
Taupier-Letage, I.
spellingShingle Olmedo, Estrella
Alvera-Azcárate, Aida
Turiel, Antonio
Taupier-Letage, I.
Enhanced SMOS Sea Surface Salinity in the Western Mediterranean Sea: accuracy and mesoscale structures description
author_facet Olmedo, Estrella
Alvera-Azcárate, Aida
Turiel, Antonio
Taupier-Letage, I.
author_sort Olmedo, Estrella
title Enhanced SMOS Sea Surface Salinity in the Western Mediterranean Sea: accuracy and mesoscale structures description
title_short Enhanced SMOS Sea Surface Salinity in the Western Mediterranean Sea: accuracy and mesoscale structures description
title_full Enhanced SMOS Sea Surface Salinity in the Western Mediterranean Sea: accuracy and mesoscale structures description
title_fullStr Enhanced SMOS Sea Surface Salinity in the Western Mediterranean Sea: accuracy and mesoscale structures description
title_full_unstemmed Enhanced SMOS Sea Surface Salinity in the Western Mediterranean Sea: accuracy and mesoscale structures description
title_sort enhanced smos sea surface salinity in the western mediterranean sea: accuracy and mesoscale structures description
publisher European Geosciences Union
publishDate 2018
url http://hdl.handle.net/10261/185268
genre North Atlantic
genre_facet North Atlantic
op_relation Publisher's version
https://meetingorganizer.copernicus.org/EGU2018/orals/26767

issn: 1607-7962
Geophysical Research Abstracts 20: EGU2018-7919 (2018)
http://hdl.handle.net/10261/185268
op_rights open
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