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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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 |
_version_ |
1766297737208266752 |