Winter Sentinel-1 Backscatter as a Predictor of Spring Arctic Sea Ice Melt Pond Fraction

Spring melt pond fraction (fp) has been shown to influence September sea ice extent and, with a growing need to improve melt pond physics in climate and forecast models, observations at large spatial scales are needed. We present a novel technique for estimating fp on sea ice at high spatial resolut...

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Published in:Geophysical Research Letters
Main Authors: Scharien, Randall K., Segal, Rebecca, Nasonova, Sasha, Nandan, Vishnu, Howell, Stephen E. L., Haas, Christian
Format: Article in Journal/Newspaper
Language:English
Published: Geophysical Research Letters 2017
Subjects:
Online Access:http://hdl.handle.net/1828/10645
https://doi.org/10.1002/2017GL075547
id ftuvicpubl:oai:dspace.library.uvic.ca:1828/10645
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spelling ftuvicpubl:oai:dspace.library.uvic.ca:1828/10645 2023-05-15T14:25:19+02:00 Winter Sentinel-1 Backscatter as a Predictor of Spring Arctic Sea Ice Melt Pond Fraction Scharien, Randall K. Segal, Rebecca Nasonova, Sasha Nandan, Vishnu Howell, Stephen E. L. Haas, Christian 2017 application/pdf http://hdl.handle.net/1828/10645 https://doi.org/10.1002/2017GL075547 en eng Geophysical Research Letters Scharien, R. K.; Segal, R.; Nasonova, S.; Nandan, V.; Howell, S. E. L.; & Haas, C. (2017). Winter Sentinel-1 backscatter as a predictor of spring Arctic sea ice melt pond fraction. Geophysical Research Letters, 44(24). DOI:10.1002/2017GL075547 https://doi.org/10.1002/2017GL075547 http://hdl.handle.net/1828/10645 sea ice melt ponds microwave backscatter Sentinel-1 seasonal forecast Article 2017 ftuvicpubl https://doi.org/10.1002/2017GL075547 2022-05-19T06:11:17Z Spring melt pond fraction (fp) has been shown to influence September sea ice extent and, with a growing need to improve melt pond physics in climate and forecast models, observations at large spatial scales are needed. We present a novel technique for estimating fp on sea ice at high spatial resolution from the Sentinel‐1 satellite during the winter period leading up to spring melt. A strong correlation (r = −0.85) is found between winter radar backscatter and fp from first‐year and multiyear sea ice data collected in the Canadian Arctic Archipelago (CAA) in 2015. Observations made in the CAA in 2016 are used to validate a fp retrieval algorithm, and a fp prediction for the CAA in 2017 is made. The method is effective using the horizontal transmit and receive polarization channel only and shows promise for providing seasonal, pan‐Arctic, fp maps for improved understanding of melt pond distributions and forecast model skill. Data collection and analysis were supported by funds from Natural Sciences and Engineering Research Council (NSERC) Discovery Grant (DG), Marine Environmental Observation, Prediction, and Response Network (MEOPAR), and the Changing Earth Science Network, part of the European Space Agency's Support To Science Element (STSE). The authors declare no financial conflicts of interests. Sentinel-1 data are available from the online database Copernicus Open Access Hub (https://scihub.copernicus.eu/). GeoEye-1 data are available at a cost from the DigitalGlobe database (https://browse.digitalglobe.com/). Supporting data are included as Data Set S1. Under certain terms and conditions, GeoEye-1 data may be available free of charge from the European Space Agency. Faculty Reviewed Article in Journal/Newspaper Arctic Arctic Archipelago Arctic Canadian Arctic Archipelago Sea ice University of Victoria (Canada): UVicDSpace Arctic Canadian Arctic Archipelago The Sentinel ENVELOPE(73.317,73.317,-52.983,-52.983) Geophysical Research Letters 44 24
institution Open Polar
collection University of Victoria (Canada): UVicDSpace
op_collection_id ftuvicpubl
language English
topic sea ice
melt ponds
microwave backscatter
Sentinel-1
seasonal forecast
spellingShingle sea ice
melt ponds
microwave backscatter
Sentinel-1
seasonal forecast
Scharien, Randall K.
Segal, Rebecca
Nasonova, Sasha
Nandan, Vishnu
Howell, Stephen E. L.
Haas, Christian
Winter Sentinel-1 Backscatter as a Predictor of Spring Arctic Sea Ice Melt Pond Fraction
topic_facet sea ice
melt ponds
microwave backscatter
Sentinel-1
seasonal forecast
description Spring melt pond fraction (fp) has been shown to influence September sea ice extent and, with a growing need to improve melt pond physics in climate and forecast models, observations at large spatial scales are needed. We present a novel technique for estimating fp on sea ice at high spatial resolution from the Sentinel‐1 satellite during the winter period leading up to spring melt. A strong correlation (r = −0.85) is found between winter radar backscatter and fp from first‐year and multiyear sea ice data collected in the Canadian Arctic Archipelago (CAA) in 2015. Observations made in the CAA in 2016 are used to validate a fp retrieval algorithm, and a fp prediction for the CAA in 2017 is made. The method is effective using the horizontal transmit and receive polarization channel only and shows promise for providing seasonal, pan‐Arctic, fp maps for improved understanding of melt pond distributions and forecast model skill. Data collection and analysis were supported by funds from Natural Sciences and Engineering Research Council (NSERC) Discovery Grant (DG), Marine Environmental Observation, Prediction, and Response Network (MEOPAR), and the Changing Earth Science Network, part of the European Space Agency's Support To Science Element (STSE). The authors declare no financial conflicts of interests. Sentinel-1 data are available from the online database Copernicus Open Access Hub (https://scihub.copernicus.eu/). GeoEye-1 data are available at a cost from the DigitalGlobe database (https://browse.digitalglobe.com/). Supporting data are included as Data Set S1. Under certain terms and conditions, GeoEye-1 data may be available free of charge from the European Space Agency. Faculty Reviewed
format Article in Journal/Newspaper
author Scharien, Randall K.
Segal, Rebecca
Nasonova, Sasha
Nandan, Vishnu
Howell, Stephen E. L.
Haas, Christian
author_facet Scharien, Randall K.
Segal, Rebecca
Nasonova, Sasha
Nandan, Vishnu
Howell, Stephen E. L.
Haas, Christian
author_sort Scharien, Randall K.
title Winter Sentinel-1 Backscatter as a Predictor of Spring Arctic Sea Ice Melt Pond Fraction
title_short Winter Sentinel-1 Backscatter as a Predictor of Spring Arctic Sea Ice Melt Pond Fraction
title_full Winter Sentinel-1 Backscatter as a Predictor of Spring Arctic Sea Ice Melt Pond Fraction
title_fullStr Winter Sentinel-1 Backscatter as a Predictor of Spring Arctic Sea Ice Melt Pond Fraction
title_full_unstemmed Winter Sentinel-1 Backscatter as a Predictor of Spring Arctic Sea Ice Melt Pond Fraction
title_sort winter sentinel-1 backscatter as a predictor of spring arctic sea ice melt pond fraction
publisher Geophysical Research Letters
publishDate 2017
url http://hdl.handle.net/1828/10645
https://doi.org/10.1002/2017GL075547
long_lat ENVELOPE(73.317,73.317,-52.983,-52.983)
geographic Arctic
Canadian Arctic Archipelago
The Sentinel
geographic_facet Arctic
Canadian Arctic Archipelago
The Sentinel
genre Arctic
Arctic Archipelago
Arctic
Canadian Arctic Archipelago
Sea ice
genre_facet Arctic
Arctic Archipelago
Arctic
Canadian Arctic Archipelago
Sea ice
op_relation Scharien, R. K.; Segal, R.; Nasonova, S.; Nandan, V.; Howell, S. E. L.; & Haas, C. (2017). Winter Sentinel-1 backscatter as a predictor of spring Arctic sea ice melt pond fraction. Geophysical Research Letters, 44(24). DOI:10.1002/2017GL075547
https://doi.org/10.1002/2017GL075547
http://hdl.handle.net/1828/10645
op_doi https://doi.org/10.1002/2017GL075547
container_title Geophysical Research Letters
container_volume 44
container_issue 24
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