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...

Full description

Bibliographic Details
Published in:Remote Sensing
Main Authors: Young-Sun Son, Hyun-cheol Kim, Sung Jae Lee
Format: Text
Language:English
Published: Multidisciplinary Digital Publishing Institute 2018
Subjects:
Online Access:https://doi.org/10.3390/rs10050662
id ftmdpi:oai:mdpi.com:/2072-4292/10/5/662/
record_format openpolar
spelling ftmdpi:oai:mdpi.com:/2072-4292/10/5/662/ 2023-11-12T04:11:53+01:00 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
institution Open Polar
collection MDPI Open Access Publishing
op_collection_id ftmdpi
language English
topic ice surface temperature (IST)
sea ice
Arctic coast
ASTER
MODIS
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
topic_facet ice surface temperature (IST)
sea ice
Arctic coast
ASTER
MODIS
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
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 Multidisciplinary Digital Publishing Institute
publishDate 2018
url https://doi.org/10.3390/rs10050662
op_coverage agris
geographic Arctic
geographic_facet Arctic
genre Arctic
Sea ice
Alaska
genre_facet Arctic
Sea ice
Alaska
op_source Remote Sensing
Volume 10
Issue 5
Pages: 662
op_relation Ocean Remote Sensing
https://dx.doi.org/10.3390/rs10050662
op_rights https://creativecommons.org/licenses/by/4.0/
op_doi https://doi.org/10.3390/rs10050662
container_title Remote Sensing
container_volume 10
container_issue 5
container_start_page 662
_version_ 1782330753364787200