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...
Published in: | Remote Sensing |
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Main Authors: | , , |
Format: | Text |
Language: | English |
Published: |
Multidisciplinary Digital Publishing Institute
2018
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Subjects: | |
Online Access: | https://doi.org/10.3390/rs10050662 |
_version_ | 1821818516527906816 |
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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 |
collection | MDPI Open Access Publishing |
container_issue | 5 |
container_start_page | 662 |
container_title | Remote Sensing |
container_volume | 10 |
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 | Text |
genre | Arctic Sea ice Alaska |
genre_facet | Arctic Sea ice Alaska |
geographic | Arctic |
geographic_facet | Arctic |
id | ftmdpi:oai:mdpi.com:/2072-4292/10/5/662/ |
institution | Open Polar |
language | English |
op_collection_id | ftmdpi |
op_coverage | agris |
op_doi | https://doi.org/10.3390/rs10050662 |
op_relation | Ocean Remote Sensing https://dx.doi.org/10.3390/rs10050662 |
op_rights | https://creativecommons.org/licenses/by/4.0/ |
op_source | Remote Sensing Volume 10 Issue 5 Pages: 662 |
publishDate | 2018 |
publisher | Multidisciplinary Digital Publishing Institute |
record_format | openpolar |
spelling | ftmdpi:oai:mdpi.com:/2072-4292/10/5/662/ 2025-01-16T20:23:56+00:00 ASTER-Derived High-Resolution Ice Surface Temperature for the Arctic Coast Young-Sun Son Hyun-cheol Kim Sung Jae Lee agris 2018-04-24 application/pdf https://doi.org/10.3390/rs10050662 eng eng Multidisciplinary Digital Publishing Institute Ocean Remote Sensing https://dx.doi.org/10.3390/rs10050662 https://creativecommons.org/licenses/by/4.0/ Remote Sensing Volume 10 Issue 5 Pages: 662 ice surface temperature (IST) sea ice Arctic coast ASTER MODIS Text 2018 ftmdpi https://doi.org/10.3390/rs10050662 2023-10-22T23:54:21Z 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. Text Arctic Sea ice Alaska MDPI Open Access Publishing Arctic Remote Sensing 10 5 662 |
spellingShingle | ice surface temperature (IST) sea ice Arctic coast ASTER MODIS Young-Sun Son Hyun-cheol Kim Sung Jae Lee ASTER-Derived High-Resolution Ice Surface Temperature for the Arctic Coast |
title | 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_short | ASTER-Derived High-Resolution Ice Surface Temperature for the Arctic Coast |
title_sort | aster-derived high-resolution ice surface temperature for the arctic coast |
topic | ice surface temperature (IST) sea ice Arctic coast ASTER MODIS |
topic_facet | ice surface temperature (IST) sea ice Arctic coast ASTER MODIS |
url | https://doi.org/10.3390/rs10050662 |