Change in the Recent Warming Trend of Sea Surface Temperature in the East Sea (Sea of Japan) over Decades (1982–2018)

Long-term trends of sea surface temperature (SST) of the East Sea (Sea of Japan, EJS) were estimated by using 37-year-long satellite data, for the observation period from 1982 to 2018. Overall, the SST tended to increase with time, for all analyzed regions. However, the warming trend was steeper in...

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Published in:Remote Sensing
Main Authors: Eun-Young Lee, Kyung-Ae Park
Format: Text
Language:English
Published: Multidisciplinary Digital Publishing Institute 2019
Subjects:
Online Access:https://doi.org/10.3390/rs11222613
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spelling ftmdpi:oai:mdpi.com:/2072-4292/11/22/2613/ 2023-08-20T04:04:08+02:00 Change in the Recent Warming Trend of Sea Surface Temperature in the East Sea (Sea of Japan) over Decades (1982–2018) Eun-Young Lee Kyung-Ae Park agris 2019-11-07 application/pdf https://doi.org/10.3390/rs11222613 EN eng Multidisciplinary Digital Publishing Institute https://dx.doi.org/10.3390/rs11222613 https://creativecommons.org/licenses/by/4.0/ Remote Sensing; Volume 11; Issue 22; Pages: 2613 sea surface temperature (SST) warming trend SST cooling East Sea (Sea of Japan) Arctic Oscillation Text 2019 ftmdpi https://doi.org/10.3390/rs11222613 2023-07-31T22:46:26Z Long-term trends of sea surface temperature (SST) of the East Sea (Sea of Japan, EJS) were estimated by using 37-year-long satellite data, for the observation period from 1982 to 2018. Overall, the SST tended to increase with time, for all analyzed regions. However, the warming trend was steeper in the earlier decades since the 1980s and slowed down during the recent two decades. Based on the analysis of the occurrence of events with extreme SST (high in the summertime and low in the wintertime), a shift toward the more frequent occurrence of events with extremely high SST and the less frequent occurrence of events with extremely low SST has been observed. This supports the observations of the consistent warming of the EJS. However, seasonal trends revealed continuous SST warming in the summertime, but frequent extreme SST cooling in the wintertime, in recent decades. The observed reduction in the warming rates occurred more frequently in specific regions of the EJS, where the occurrence frequency of events with extremely low SST was unusually high in the recent decade. The recent tendency toward the SST cooling was distinctively connected with variations in the Arctic Oscillation index. This suggests that changes in the Arctic Ocean environment likely affect the recently observed SST changes in the EJS, as one of the marginal seas in the mid-latitude region far from the polar region. Text Arctic Arctic Ocean MDPI Open Access Publishing Arctic Arctic Ocean Remote Sensing 11 22 2613
institution Open Polar
collection MDPI Open Access Publishing
op_collection_id ftmdpi
language English
topic sea surface temperature (SST)
warming trend
SST cooling
East Sea (Sea of Japan)
Arctic Oscillation
spellingShingle sea surface temperature (SST)
warming trend
SST cooling
East Sea (Sea of Japan)
Arctic Oscillation
Eun-Young Lee
Kyung-Ae Park
Change in the Recent Warming Trend of Sea Surface Temperature in the East Sea (Sea of Japan) over Decades (1982–2018)
topic_facet sea surface temperature (SST)
warming trend
SST cooling
East Sea (Sea of Japan)
Arctic Oscillation
description Long-term trends of sea surface temperature (SST) of the East Sea (Sea of Japan, EJS) were estimated by using 37-year-long satellite data, for the observation period from 1982 to 2018. Overall, the SST tended to increase with time, for all analyzed regions. However, the warming trend was steeper in the earlier decades since the 1980s and slowed down during the recent two decades. Based on the analysis of the occurrence of events with extreme SST (high in the summertime and low in the wintertime), a shift toward the more frequent occurrence of events with extremely high SST and the less frequent occurrence of events with extremely low SST has been observed. This supports the observations of the consistent warming of the EJS. However, seasonal trends revealed continuous SST warming in the summertime, but frequent extreme SST cooling in the wintertime, in recent decades. The observed reduction in the warming rates occurred more frequently in specific regions of the EJS, where the occurrence frequency of events with extremely low SST was unusually high in the recent decade. The recent tendency toward the SST cooling was distinctively connected with variations in the Arctic Oscillation index. This suggests that changes in the Arctic Ocean environment likely affect the recently observed SST changes in the EJS, as one of the marginal seas in the mid-latitude region far from the polar region.
format Text
author Eun-Young Lee
Kyung-Ae Park
author_facet Eun-Young Lee
Kyung-Ae Park
author_sort Eun-Young Lee
title Change in the Recent Warming Trend of Sea Surface Temperature in the East Sea (Sea of Japan) over Decades (1982–2018)
title_short Change in the Recent Warming Trend of Sea Surface Temperature in the East Sea (Sea of Japan) over Decades (1982–2018)
title_full Change in the Recent Warming Trend of Sea Surface Temperature in the East Sea (Sea of Japan) over Decades (1982–2018)
title_fullStr Change in the Recent Warming Trend of Sea Surface Temperature in the East Sea (Sea of Japan) over Decades (1982–2018)
title_full_unstemmed Change in the Recent Warming Trend of Sea Surface Temperature in the East Sea (Sea of Japan) over Decades (1982–2018)
title_sort change in the recent warming trend of sea surface temperature in the east sea (sea of japan) over decades (1982–2018)
publisher Multidisciplinary Digital Publishing Institute
publishDate 2019
url https://doi.org/10.3390/rs11222613
op_coverage agris
geographic Arctic
Arctic Ocean
geographic_facet Arctic
Arctic Ocean
genre Arctic
Arctic Ocean
genre_facet Arctic
Arctic Ocean
op_source Remote Sensing; Volume 11; Issue 22; Pages: 2613
op_relation https://dx.doi.org/10.3390/rs11222613
op_rights https://creativecommons.org/licenses/by/4.0/
op_doi https://doi.org/10.3390/rs11222613
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