Are Sea Surface Temperature Variations in the Kuroshio Extension and Subarctic Frontal Zones in the Western North Pacific Ocean Coherent?

The western North Pacific region is one of the centers of action of decadal time scale variations in the atmosphere and ocean, and also oceanic ecosystem can be strongly influenced by the variations. One of the key variable of the decadal variations is sea surface temperature (SST) that varies as a...

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Main Authors: Nonaka, Masami, Nakamura, Hisashi
Format: Conference Object
Language:English
Published: 21st Century COE for Neo-Science of Natural History, Hokkaido University
Subjects:
450
Online Access:http://hdl.handle.net/2115/38466
id fthokunivhus:oai:eprints.lib.hokudai.ac.jp:2115/38466
record_format openpolar
spelling fthokunivhus:oai:eprints.lib.hokudai.ac.jp:2115/38466 2023-05-15T18:28:13+02:00 Are Sea Surface Temperature Variations in the Kuroshio Extension and Subarctic Frontal Zones in the Western North Pacific Ocean Coherent? Nonaka, Masami Nakamura, Hisashi http://hdl.handle.net/2115/38466 eng eng 21st Century COE for Neo-Science of Natural History, Hokkaido University Edited by Hisatake Okada, Shunsuke F. Mawatari, Noriyuki Suzuki, Pitambar Gautam. ISBN: 978-4-9903990-0-9 http://hdl.handle.net/2115/38466 International Symposium, "The Origin and Evolution of Natural Diversity", Sapporo North Pacific Sea surface temperature Decadal variability 450 proceedings fthokunivhus 2022-11-18T01:01:45Z The western North Pacific region is one of the centers of action of decadal time scale variations in the atmosphere and ocean, and also oceanic ecosystem can be strongly influenced by the variations. One of the key variable of the decadal variations is sea surface temperature (SST) that varies as a result of interaction between the atmosphere and ocean. To improve our understanding of the key element, SST variaions in the two frontal zones in the western North Pacific Ocean, the Kuroshio Extension and subarctic frontal zones, are investigated on the basis of an in situ observational dataset. Interannual-to-decadal variations in these two frontal zones are not highly correlated, indicating that to some extent different mechanisms induce the SST variations in the frontal zones and those two frontal zone cannot be considered as a single frontal zone as has been done in most of previous studies. Meanwhile, the results are consistent with the recent studies that suggest different mechanisms for the variations in the two frontal zones on the basis of a solution to an eddy-resolving, i.e., very high horizontal resolution, ocean general circulation model. International Symposium, "The Origin and Evolution of Natural Diversity". 1–5 October 2007. Sapporo, Japan. Conference Object Subarctic Hokkaido University Collection of Scholarly and Academic Papers (HUSCAP) Pacific
institution Open Polar
collection Hokkaido University Collection of Scholarly and Academic Papers (HUSCAP)
op_collection_id fthokunivhus
language English
topic North Pacific
Sea surface temperature
Decadal variability
450
spellingShingle North Pacific
Sea surface temperature
Decadal variability
450
Nonaka, Masami
Nakamura, Hisashi
Are Sea Surface Temperature Variations in the Kuroshio Extension and Subarctic Frontal Zones in the Western North Pacific Ocean Coherent?
topic_facet North Pacific
Sea surface temperature
Decadal variability
450
description The western North Pacific region is one of the centers of action of decadal time scale variations in the atmosphere and ocean, and also oceanic ecosystem can be strongly influenced by the variations. One of the key variable of the decadal variations is sea surface temperature (SST) that varies as a result of interaction between the atmosphere and ocean. To improve our understanding of the key element, SST variaions in the two frontal zones in the western North Pacific Ocean, the Kuroshio Extension and subarctic frontal zones, are investigated on the basis of an in situ observational dataset. Interannual-to-decadal variations in these two frontal zones are not highly correlated, indicating that to some extent different mechanisms induce the SST variations in the frontal zones and those two frontal zone cannot be considered as a single frontal zone as has been done in most of previous studies. Meanwhile, the results are consistent with the recent studies that suggest different mechanisms for the variations in the two frontal zones on the basis of a solution to an eddy-resolving, i.e., very high horizontal resolution, ocean general circulation model. International Symposium, "The Origin and Evolution of Natural Diversity". 1–5 October 2007. Sapporo, Japan.
format Conference Object
author Nonaka, Masami
Nakamura, Hisashi
author_facet Nonaka, Masami
Nakamura, Hisashi
author_sort Nonaka, Masami
title Are Sea Surface Temperature Variations in the Kuroshio Extension and Subarctic Frontal Zones in the Western North Pacific Ocean Coherent?
title_short Are Sea Surface Temperature Variations in the Kuroshio Extension and Subarctic Frontal Zones in the Western North Pacific Ocean Coherent?
title_full Are Sea Surface Temperature Variations in the Kuroshio Extension and Subarctic Frontal Zones in the Western North Pacific Ocean Coherent?
title_fullStr Are Sea Surface Temperature Variations in the Kuroshio Extension and Subarctic Frontal Zones in the Western North Pacific Ocean Coherent?
title_full_unstemmed Are Sea Surface Temperature Variations in the Kuroshio Extension and Subarctic Frontal Zones in the Western North Pacific Ocean Coherent?
title_sort are sea surface temperature variations in the kuroshio extension and subarctic frontal zones in the western north pacific ocean coherent?
publisher 21st Century COE for Neo-Science of Natural History, Hokkaido University
url http://hdl.handle.net/2115/38466
geographic Pacific
geographic_facet Pacific
genre Subarctic
genre_facet Subarctic
op_relation Edited by Hisatake Okada, Shunsuke F. Mawatari, Noriyuki Suzuki, Pitambar Gautam. ISBN: 978-4-9903990-0-9
http://hdl.handle.net/2115/38466
International Symposium, "The Origin and Evolution of Natural Diversity", Sapporo
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