Interannual variation in solar heating in the Chukchi Sea, Arctic Ocean

Solar heating in summer in the Chukchi Sea was estimated using satellite-derived sea-ice concentration data and reanalysis shortwave radiation data. The shortwave radiation was validated by in-situ data obtained by the R/V Mirai and NCEP-CFSR/CFSv2 was found to reproduce in-situ data accurately comp...

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Published in:Polar Science
Format: Article in Journal/Newspaper
Language:English
Published: 2018
Subjects:
Online Access:https://nipr.repo.nii.ac.jp/?action=repository_uri&item_id=15101
http://id.nii.ac.jp/1291/00015011/
id ftnipr:oai:nipr.repo.nii.ac.jp:00015101
record_format openpolar
spelling ftnipr:oai:nipr.repo.nii.ac.jp:00015101 2023-05-15T14:29:09+02:00 Interannual variation in solar heating in the Chukchi Sea, Arctic Ocean 2018-09 https://nipr.repo.nii.ac.jp/?action=repository_uri&item_id=15101 http://id.nii.ac.jp/1291/00015011/ en eng https://doi.org/10.1016/j.polar.2018.06.003 https://nipr.repo.nii.ac.jp/?action=repository_uri&item_id=15101 http://id.nii.ac.jp/1291/00015011/ Polar Science, 17, 33-39(2018-09) 18739652 Solar heating Chukchi sea Interannual variation Journal Article 2018 ftnipr https://doi.org/10.1016/j.polar.2018.06.003 2022-12-03T19:43:10Z Solar heating in summer in the Chukchi Sea was estimated using satellite-derived sea-ice concentration data and reanalysis shortwave radiation data. The shortwave radiation was validated by in-situ data obtained by the R/V Mirai and NCEP-CFSR/CFSv2 was found to reproduce in-situ data accurately compared with NCEP/NCAR Reanalysis 1 and ERA-Interim. Solar heating integrated over the Chukchi Sea in summer varied interannually from 3.6 × 1020 J in 2000 to 6.7 × 1020 J in 2015, and was up to twice the northward heat flux through the Bering Strait. The total heating in the Chukchi Sea implies that the heat in the Chukchi Sea provided by northward heat flux through the Bering Strait is amplified by solar heating in the Chukchi Sea. We further compared these heat fluxes into the Chukchi Sea with the summertime northward heat flux through Barrow Canyon, an indicator of heat flux from the Chukchi Sea to the Arctic basin. The northward heat flux through Barrow Canyon was affected by the interannual variation of solar heating in the eastern Chukchi Sea. These results imply that modification of Pacific water in the Chukchi Sea by solar heating plays an important role in the interannual variation in heat transport from the Chukchi Sea to the western Arctic basin. Article in Journal/Newspaper Arctic Basin Arctic Arctic Ocean Bering Strait Chukchi Chukchi Sea Polar Science Polar Science Sea ice National Institute of Polar Research Repository, Japan Arctic Arctic Ocean Barrow Canyon ENVELOPE(-154.000,-154.000,72.500,72.500) Bering Strait Chukchi Sea Pacific Polar Science 17 33 39
institution Open Polar
collection National Institute of Polar Research Repository, Japan
op_collection_id ftnipr
language English
topic Solar heating
Chukchi sea
Interannual variation
spellingShingle Solar heating
Chukchi sea
Interannual variation
Interannual variation in solar heating in the Chukchi Sea, Arctic Ocean
topic_facet Solar heating
Chukchi sea
Interannual variation
description Solar heating in summer in the Chukchi Sea was estimated using satellite-derived sea-ice concentration data and reanalysis shortwave radiation data. The shortwave radiation was validated by in-situ data obtained by the R/V Mirai and NCEP-CFSR/CFSv2 was found to reproduce in-situ data accurately compared with NCEP/NCAR Reanalysis 1 and ERA-Interim. Solar heating integrated over the Chukchi Sea in summer varied interannually from 3.6 × 1020 J in 2000 to 6.7 × 1020 J in 2015, and was up to twice the northward heat flux through the Bering Strait. The total heating in the Chukchi Sea implies that the heat in the Chukchi Sea provided by northward heat flux through the Bering Strait is amplified by solar heating in the Chukchi Sea. We further compared these heat fluxes into the Chukchi Sea with the summertime northward heat flux through Barrow Canyon, an indicator of heat flux from the Chukchi Sea to the Arctic basin. The northward heat flux through Barrow Canyon was affected by the interannual variation of solar heating in the eastern Chukchi Sea. These results imply that modification of Pacific water in the Chukchi Sea by solar heating plays an important role in the interannual variation in heat transport from the Chukchi Sea to the western Arctic basin.
format Article in Journal/Newspaper
title Interannual variation in solar heating in the Chukchi Sea, Arctic Ocean
title_short Interannual variation in solar heating in the Chukchi Sea, Arctic Ocean
title_full Interannual variation in solar heating in the Chukchi Sea, Arctic Ocean
title_fullStr Interannual variation in solar heating in the Chukchi Sea, Arctic Ocean
title_full_unstemmed Interannual variation in solar heating in the Chukchi Sea, Arctic Ocean
title_sort interannual variation in solar heating in the chukchi sea, arctic ocean
publishDate 2018
url https://nipr.repo.nii.ac.jp/?action=repository_uri&item_id=15101
http://id.nii.ac.jp/1291/00015011/
long_lat ENVELOPE(-154.000,-154.000,72.500,72.500)
geographic Arctic
Arctic Ocean
Barrow Canyon
Bering Strait
Chukchi Sea
Pacific
geographic_facet Arctic
Arctic Ocean
Barrow Canyon
Bering Strait
Chukchi Sea
Pacific
genre Arctic Basin
Arctic
Arctic Ocean
Bering Strait
Chukchi
Chukchi Sea
Polar Science
Polar Science
Sea ice
genre_facet Arctic Basin
Arctic
Arctic Ocean
Bering Strait
Chukchi
Chukchi Sea
Polar Science
Polar Science
Sea ice
op_relation https://doi.org/10.1016/j.polar.2018.06.003
https://nipr.repo.nii.ac.jp/?action=repository_uri&item_id=15101
http://id.nii.ac.jp/1291/00015011/
Polar Science, 17, 33-39(2018-09)
18739652
op_doi https://doi.org/10.1016/j.polar.2018.06.003
container_title Polar Science
container_volume 17
container_start_page 33
op_container_end_page 39
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