Spatial Scales of Sea Surface Salinity Subfootprint Variability in the SPURS Regions

Subfootprint variability (SFV), or representativeness error, is variability within the footprint of a satellite that can impact validation by comparison of in situ and remote sensing data. This study seeks to determine the size of the sea surface salinity (SSS) SFV as a function of footprint size in...

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Published in:Remote Sensing
Main Authors: Frederick M. Bingham, Zhijin Li
Format: Article in Journal/Newspaper
Language:English
Published: MDPI AG 2020
Subjects:
Q
Online Access:https://doi.org/10.3390/rs12233996
https://doaj.org/article/bccd8fac8b114ecbbf0c687dec504ea0
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spelling ftdoajarticles:oai:doaj.org/article:bccd8fac8b114ecbbf0c687dec504ea0 2024-01-07T09:45:10+01:00 Spatial Scales of Sea Surface Salinity Subfootprint Variability in the SPURS Regions Frederick M. Bingham Zhijin Li 2020-12-01T00:00:00Z https://doi.org/10.3390/rs12233996 https://doaj.org/article/bccd8fac8b114ecbbf0c687dec504ea0 EN eng MDPI AG https://www.mdpi.com/2072-4292/12/23/3996 https://doaj.org/toc/2072-4292 doi:10.3390/rs12233996 2072-4292 https://doaj.org/article/bccd8fac8b114ecbbf0c687dec504ea0 Remote Sensing, Vol 12, Iss 23, p 3996 (2020) surface salinity remote sensing subfootprint variability representativeness error spatial scale Science Q article 2020 ftdoajarticles https://doi.org/10.3390/rs12233996 2023-12-10T01:48:43Z Subfootprint variability (SFV), or representativeness error, is variability within the footprint of a satellite that can impact validation by comparison of in situ and remote sensing data. This study seeks to determine the size of the sea surface salinity (SSS) SFV as a function of footprint size in two regions that were heavily sampled with in situ data. The Salinity Processes in the Upper-ocean Regional Studies-1 (SPURS-1) experiment was conducted in the subtropical North Atlantic in the period 2012–2013, whereas the SPURS-2 study was conducted in the tropical eastern North Pacific in the period 2016–2017. SSS SFV was also computed using a high-resolution regional model based on the Regional Ocean Modeling System (ROMS). We computed SFV at footprint sizes ranging from 20 to 100 km for both regions. SFV is strongly seasonal, but for different reasons in the two regions. In the SPURS-1 region, the meso- and submesoscale variability seemed to control the size of the SFV. In the SPURS-2 region, the SFV is much larger than SPURS-1 and controlled by patchy rainfall. Article in Journal/Newspaper North Atlantic Directory of Open Access Journals: DOAJ Articles Pacific Remote Sensing 12 23 3996
institution Open Polar
collection Directory of Open Access Journals: DOAJ Articles
op_collection_id ftdoajarticles
language English
topic surface salinity
remote sensing
subfootprint variability
representativeness error
spatial scale
Science
Q
spellingShingle surface salinity
remote sensing
subfootprint variability
representativeness error
spatial scale
Science
Q
Frederick M. Bingham
Zhijin Li
Spatial Scales of Sea Surface Salinity Subfootprint Variability in the SPURS Regions
topic_facet surface salinity
remote sensing
subfootprint variability
representativeness error
spatial scale
Science
Q
description Subfootprint variability (SFV), or representativeness error, is variability within the footprint of a satellite that can impact validation by comparison of in situ and remote sensing data. This study seeks to determine the size of the sea surface salinity (SSS) SFV as a function of footprint size in two regions that were heavily sampled with in situ data. The Salinity Processes in the Upper-ocean Regional Studies-1 (SPURS-1) experiment was conducted in the subtropical North Atlantic in the period 2012–2013, whereas the SPURS-2 study was conducted in the tropical eastern North Pacific in the period 2016–2017. SSS SFV was also computed using a high-resolution regional model based on the Regional Ocean Modeling System (ROMS). We computed SFV at footprint sizes ranging from 20 to 100 km for both regions. SFV is strongly seasonal, but for different reasons in the two regions. In the SPURS-1 region, the meso- and submesoscale variability seemed to control the size of the SFV. In the SPURS-2 region, the SFV is much larger than SPURS-1 and controlled by patchy rainfall.
format Article in Journal/Newspaper
author Frederick M. Bingham
Zhijin Li
author_facet Frederick M. Bingham
Zhijin Li
author_sort Frederick M. Bingham
title Spatial Scales of Sea Surface Salinity Subfootprint Variability in the SPURS Regions
title_short Spatial Scales of Sea Surface Salinity Subfootprint Variability in the SPURS Regions
title_full Spatial Scales of Sea Surface Salinity Subfootprint Variability in the SPURS Regions
title_fullStr Spatial Scales of Sea Surface Salinity Subfootprint Variability in the SPURS Regions
title_full_unstemmed Spatial Scales of Sea Surface Salinity Subfootprint Variability in the SPURS Regions
title_sort spatial scales of sea surface salinity subfootprint variability in the spurs regions
publisher MDPI AG
publishDate 2020
url https://doi.org/10.3390/rs12233996
https://doaj.org/article/bccd8fac8b114ecbbf0c687dec504ea0
geographic Pacific
geographic_facet Pacific
genre North Atlantic
genre_facet North Atlantic
op_source Remote Sensing, Vol 12, Iss 23, p 3996 (2020)
op_relation https://www.mdpi.com/2072-4292/12/23/3996
https://doaj.org/toc/2072-4292
doi:10.3390/rs12233996
2072-4292
https://doaj.org/article/bccd8fac8b114ecbbf0c687dec504ea0
op_doi https://doi.org/10.3390/rs12233996
container_title Remote Sensing
container_volume 12
container_issue 23
container_start_page 3996
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