ASTER-Derived High-Resolution Ice Surface Temperature for the Arctic Coast

Ice surface temperature (IST) controls the rate of sea ice growth and the heat exchange between the atmosphere and ocean. In this study, high-resolution IST using the Advanced Spaceborne Thermal Emission and Reflection radiometer (ASTER) thermal infrared region (TIR) images was retrieved to observe...

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Published in:Remote Sensing
Main Authors: Young-Sun Son, Hyun-cheol Kim, Sung Jae Lee
Format: Article in Journal/Newspaper
Language:English
Published: MDPI AG 2018
Subjects:
Q
Online Access:https://doi.org/10.3390/rs10050662
https://doaj.org/article/27990a498eeb43f3a0d58fd1495553c1
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spelling ftdoajarticles:oai:doaj.org/article:27990a498eeb43f3a0d58fd1495553c1 2023-05-15T14:53:33+02:00 ASTER-Derived High-Resolution Ice Surface Temperature for the Arctic Coast Young-Sun Son Hyun-cheol Kim Sung Jae Lee 2018-04-01T00:00:00Z https://doi.org/10.3390/rs10050662 https://doaj.org/article/27990a498eeb43f3a0d58fd1495553c1 EN eng MDPI AG http://www.mdpi.com/2072-4292/10/5/662 https://doaj.org/toc/2072-4292 2072-4292 doi:10.3390/rs10050662 https://doaj.org/article/27990a498eeb43f3a0d58fd1495553c1 Remote Sensing, Vol 10, Iss 5, p 662 (2018) ice surface temperature (IST) sea ice Arctic coast ASTER MODIS Science Q article 2018 ftdoajarticles https://doi.org/10.3390/rs10050662 2022-12-31T16:17:42Z Ice surface temperature (IST) controls the rate of sea ice growth and the heat exchange between the atmosphere and ocean. In this study, high-resolution IST using the Advanced Spaceborne Thermal Emission and Reflection radiometer (ASTER) thermal infrared region (TIR) images was retrieved to observe the thermal change of coastal sea ice. The regression coefficients of the multi-channel equation using ASTER brightness temperatures ( B T ) and MODIS ISTs were derived. MODIS IST products (MOD29) were used as an in situ temperature substitute. The ASTER IST using five channels from band 10 ( B T 10 ) to band 14 ( B T 14 ) showed an RMSE of 0.746 K for the validation images on the Alaskan coast. The uncertainty of the two-channel ( B T 13 and B T 14 ) ASTER IST was 0.497 K, which was better than that of the five-channel. We thus concluded that the two-channel equation using ASTER B T 13 and B T 14 was an optimal model for the surface temperature retrieval of coastal sea ice. The two-channel ASTER IST showed similar accuracy at higher latitudes than in Alaska. Therefore, ASTER-derived IST with 90 m spatial resolution can be used to observe small-scale thermal variations on the sea ice surface along the Arctic coast. Article in Journal/Newspaper Arctic Sea ice Alaska Directory of Open Access Journals: DOAJ Articles Arctic Remote Sensing 10 5 662
institution Open Polar
collection Directory of Open Access Journals: DOAJ Articles
op_collection_id ftdoajarticles
language English
topic ice surface temperature (IST)
sea ice
Arctic coast
ASTER
MODIS
Science
Q
spellingShingle ice surface temperature (IST)
sea ice
Arctic coast
ASTER
MODIS
Science
Q
Young-Sun Son
Hyun-cheol Kim
Sung Jae Lee
ASTER-Derived High-Resolution Ice Surface Temperature for the Arctic Coast
topic_facet ice surface temperature (IST)
sea ice
Arctic coast
ASTER
MODIS
Science
Q
description Ice surface temperature (IST) controls the rate of sea ice growth and the heat exchange between the atmosphere and ocean. In this study, high-resolution IST using the Advanced Spaceborne Thermal Emission and Reflection radiometer (ASTER) thermal infrared region (TIR) images was retrieved to observe the thermal change of coastal sea ice. The regression coefficients of the multi-channel equation using ASTER brightness temperatures ( B T ) and MODIS ISTs were derived. MODIS IST products (MOD29) were used as an in situ temperature substitute. The ASTER IST using five channels from band 10 ( B T 10 ) to band 14 ( B T 14 ) showed an RMSE of 0.746 K for the validation images on the Alaskan coast. The uncertainty of the two-channel ( B T 13 and B T 14 ) ASTER IST was 0.497 K, which was better than that of the five-channel. We thus concluded that the two-channel equation using ASTER B T 13 and B T 14 was an optimal model for the surface temperature retrieval of coastal sea ice. The two-channel ASTER IST showed similar accuracy at higher latitudes than in Alaska. Therefore, ASTER-derived IST with 90 m spatial resolution can be used to observe small-scale thermal variations on the sea ice surface along the Arctic coast.
format Article in Journal/Newspaper
author Young-Sun Son
Hyun-cheol Kim
Sung Jae Lee
author_facet Young-Sun Son
Hyun-cheol Kim
Sung Jae Lee
author_sort Young-Sun Son
title ASTER-Derived High-Resolution Ice Surface Temperature for the Arctic Coast
title_short ASTER-Derived High-Resolution Ice Surface Temperature for the Arctic Coast
title_full ASTER-Derived High-Resolution Ice Surface Temperature for the Arctic Coast
title_fullStr ASTER-Derived High-Resolution Ice Surface Temperature for the Arctic Coast
title_full_unstemmed ASTER-Derived High-Resolution Ice Surface Temperature for the Arctic Coast
title_sort aster-derived high-resolution ice surface temperature for the arctic coast
publisher MDPI AG
publishDate 2018
url https://doi.org/10.3390/rs10050662
https://doaj.org/article/27990a498eeb43f3a0d58fd1495553c1
geographic Arctic
geographic_facet Arctic
genre Arctic
Sea ice
Alaska
genre_facet Arctic
Sea ice
Alaska
op_source Remote Sensing, Vol 10, Iss 5, p 662 (2018)
op_relation http://www.mdpi.com/2072-4292/10/5/662
https://doaj.org/toc/2072-4292
2072-4292
doi:10.3390/rs10050662
https://doaj.org/article/27990a498eeb43f3a0d58fd1495553c1
op_doi https://doi.org/10.3390/rs10050662
container_title Remote Sensing
container_volume 10
container_issue 5
container_start_page 662
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