Cabbeling due to mixing of the Bering Strait and the Chukchi Sea waters on seasonal and climatic scale

Cabbeling due to mixing of the surface waters from the Bering Strait and the Chukchi Sea is evaluated quantitatively and variations of its impact on seasonal and climatic scale are analyzed. The cabbeling effect increases additionally the mixed water density in 0.059 kg/m3 in summer and in 0.001 kg/...

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Published in:Izvestiya TINRO
Main Author: T. R. Kilmatov
Format: Article in Journal/Newspaper
Language:Russian
Published: Transactions of the Pacific Research Institute of Fisheries and Oceanography 2022
Subjects:
Online Access:https://doi.org/10.26428/1606-9919-2022-202-409-413
https://doaj.org/article/fdbfd8f460cb4af180cab0dd31b7ab37
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spelling ftdoajarticles:oai:doaj.org/article:fdbfd8f460cb4af180cab0dd31b7ab37 2023-10-09T21:49:04+02:00 Cabbeling due to mixing of the Bering Strait and the Chukchi Sea waters on seasonal and climatic scale T. R. Kilmatov 2022-07-01T00:00:00Z https://doi.org/10.26428/1606-9919-2022-202-409-413 https://doaj.org/article/fdbfd8f460cb4af180cab0dd31b7ab37 RU rus Transactions of the Pacific Research Institute of Fisheries and Oceanography https://izvestiya.tinro-center.ru/jour/article/view/733 https://doaj.org/toc/1606-9919 https://doaj.org/toc/2658-5510 1606-9919 2658-5510 doi:10.26428/1606-9919-2022-202-409-413 https://doaj.org/article/fdbfd8f460cb4af180cab0dd31b7ab37 Известия ТИНРО, Vol 202, Iss 2, Pp 409-413 (2022) каббелинг уплотнение при смешении вод берингов пролив сезонный ход климатическая изменчивость Aquaculture. Fisheries. Angling SH1-691 article 2022 ftdoajarticles https://doi.org/10.26428/1606-9919-2022-202-409-413 2023-09-10T00:44:24Z Cabbeling due to mixing of the surface waters from the Bering Strait and the Chukchi Sea is evaluated quantitatively and variations of its impact on seasonal and climatic scale are analyzed. The cabbeling effect increases additionally the mixed water density in 0.059 kg/m3 in summer and in 0.001 kg/m3 in winter. Seasonal variation of the cabelling repeats the seasonal variation of temperature difference between the interacted water masses (ΔT ~ 5,0 оC in summer, ΔT ~ 0,5 оC in winter). This process provides additional energy for sinking of warm and salt mixed water in summer, when it penetrates far into the Arctic. In winter, the temperature difference between the mixing waters is about zero, so the cabbeling almost disappears. Both temperature and salinity have climatic trends in the Chukchi Sea that causes the climate-scale variation of the cabbeling: its impact increases in 0.002 kg/m3 per decade in summer because of climatic heating (~0,13 оC/decade) and salinity decrease (~0.04 psu/decade). Article in Journal/Newspaper Arctic Bering Strait Chukchi Chukchi Sea Берингов пролив Directory of Open Access Journals: DOAJ Articles Arctic Bering Strait Chukchi Sea Izvestiya TINRO 202 2 409 413
institution Open Polar
collection Directory of Open Access Journals: DOAJ Articles
op_collection_id ftdoajarticles
language Russian
topic каббелинг
уплотнение при смешении вод
берингов пролив
сезонный ход
климатическая изменчивость
Aquaculture. Fisheries. Angling
SH1-691
spellingShingle каббелинг
уплотнение при смешении вод
берингов пролив
сезонный ход
климатическая изменчивость
Aquaculture. Fisheries. Angling
SH1-691
T. R. Kilmatov
Cabbeling due to mixing of the Bering Strait and the Chukchi Sea waters on seasonal and climatic scale
topic_facet каббелинг
уплотнение при смешении вод
берингов пролив
сезонный ход
климатическая изменчивость
Aquaculture. Fisheries. Angling
SH1-691
description Cabbeling due to mixing of the surface waters from the Bering Strait and the Chukchi Sea is evaluated quantitatively and variations of its impact on seasonal and climatic scale are analyzed. The cabbeling effect increases additionally the mixed water density in 0.059 kg/m3 in summer and in 0.001 kg/m3 in winter. Seasonal variation of the cabelling repeats the seasonal variation of temperature difference between the interacted water masses (ΔT ~ 5,0 оC in summer, ΔT ~ 0,5 оC in winter). This process provides additional energy for sinking of warm and salt mixed water in summer, when it penetrates far into the Arctic. In winter, the temperature difference between the mixing waters is about zero, so the cabbeling almost disappears. Both temperature and salinity have climatic trends in the Chukchi Sea that causes the climate-scale variation of the cabbeling: its impact increases in 0.002 kg/m3 per decade in summer because of climatic heating (~0,13 оC/decade) and salinity decrease (~0.04 psu/decade).
format Article in Journal/Newspaper
author T. R. Kilmatov
author_facet T. R. Kilmatov
author_sort T. R. Kilmatov
title Cabbeling due to mixing of the Bering Strait and the Chukchi Sea waters on seasonal and climatic scale
title_short Cabbeling due to mixing of the Bering Strait and the Chukchi Sea waters on seasonal and climatic scale
title_full Cabbeling due to mixing of the Bering Strait and the Chukchi Sea waters on seasonal and climatic scale
title_fullStr Cabbeling due to mixing of the Bering Strait and the Chukchi Sea waters on seasonal and climatic scale
title_full_unstemmed Cabbeling due to mixing of the Bering Strait and the Chukchi Sea waters on seasonal and climatic scale
title_sort cabbeling due to mixing of the bering strait and the chukchi sea waters on seasonal and climatic scale
publisher Transactions of the Pacific Research Institute of Fisheries and Oceanography
publishDate 2022
url https://doi.org/10.26428/1606-9919-2022-202-409-413
https://doaj.org/article/fdbfd8f460cb4af180cab0dd31b7ab37
geographic Arctic
Bering Strait
Chukchi Sea
geographic_facet Arctic
Bering Strait
Chukchi Sea
genre Arctic
Bering Strait
Chukchi
Chukchi Sea
Берингов пролив
genre_facet Arctic
Bering Strait
Chukchi
Chukchi Sea
Берингов пролив
op_source Известия ТИНРО, Vol 202, Iss 2, Pp 409-413 (2022)
op_relation https://izvestiya.tinro-center.ru/jour/article/view/733
https://doaj.org/toc/1606-9919
https://doaj.org/toc/2658-5510
1606-9919
2658-5510
doi:10.26428/1606-9919-2022-202-409-413
https://doaj.org/article/fdbfd8f460cb4af180cab0dd31b7ab37
op_doi https://doi.org/10.26428/1606-9919-2022-202-409-413
container_title Izvestiya TINRO
container_volume 202
container_issue 2
container_start_page 409
op_container_end_page 413
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