Response of Influence of Internal and External Factors in the Latitudinal Sea Ice Edge Displacement in the Arctic Basin

Inter-annual climatic response of the sea ice edge latitudinal displacement in the Arctic to variability of the large-scale atmospheric circulation (the Arctic Oscillation and North Atlantic Oscillation), location of the Gulf Stream northern boundary and solar activity in 1969–2012 is studied. It is...

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Published in:Physical Oceanography
Main Authors: A.E. Bukatov, A.A. Bukatov, M.V. Babii
Format: Article in Journal/Newspaper
Language:English
Published: Federal State Budget Scientific Institution «Marine Hydrophysical Institute of RAS» 2016
Subjects:
Online Access:https://doi.org/10.22449/1573-160X-2016-6-24-31
https://doaj.org/article/6f431410e383499590f44bedcaf29fbf
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spelling ftdoajarticles:oai:doaj.org/article:6f431410e383499590f44bedcaf29fbf 2023-05-15T14:29:14+02:00 Response of Influence of Internal and External Factors in the Latitudinal Sea Ice Edge Displacement in the Arctic Basin A.E. Bukatov A.A. Bukatov M.V. Babii 2016-12-01T00:00:00Z https://doi.org/10.22449/1573-160X-2016-6-24-31 https://doaj.org/article/6f431410e383499590f44bedcaf29fbf EN eng Federal State Budget Scientific Institution «Marine Hydrophysical Institute of RAS» http://physical-oceanography.ru/repository/2016/6/en_201606_03.pdf https://doaj.org/toc/1573-160X doi:10.22449/1573-160X-2016-6-24-31 1573-160X https://doaj.org/article/6f431410e383499590f44bedcaf29fbf Physical Oceanography, Iss 6, Pp 24-31 (2016) Arctic sea ice sea ice edge dynamics of edge position Oceanography GC1-1581 article 2016 ftdoajarticles https://doi.org/10.22449/1573-160X-2016-6-24-31 2022-12-30T23:17:56Z Inter-annual climatic response of the sea ice edge latitudinal displacement in the Arctic to variability of the large-scale atmospheric circulation (the Arctic Oscillation and North Atlantic Oscillation), location of the Gulf Stream northern boundary and solar activity in 1969–2012 is studied. It is noted that the most significant ice edge latitudinal displacements in the intra-annual cycle were observed westward of Novaya Zemlya and in the Bering Strait area. It is shown that, depending on the longitudinal sector, response of the edge geographical position to changes of the atmospheric circulation and the Gulf Stream indices can be manifested both quasi-synchronously and with a delay. Exceptions are the Greenland Sea and the Norwegian Sea areas as well as the Barents Sea western part where ice edge displacements advance the Gulf Stream index variation. The correlation between the edge latitudinal displacement along its perimeter and the Wolf numbers variation is assessed. It is received that the oscillations of cross-correlation functions with a period which is close to 11-year one (Schwabe Cycle) are observed on each longitude at that. In the variations of cross-correlation functions from their average position, solar activity variation is manifested in the edge position displacement with up to two-year delay. Article in Journal/Newspaper Arctic Basin Arctic Barents Sea Bering Strait Greenland Greenland Sea North Atlantic North Atlantic oscillation Norwegian Sea Novaya Zemlya Sea ice Directory of Open Access Journals: DOAJ Articles Arctic Barents Sea Bering Strait Greenland Norwegian Sea Physical Oceanography 6
institution Open Polar
collection Directory of Open Access Journals: DOAJ Articles
op_collection_id ftdoajarticles
language English
topic Arctic
sea ice
sea ice edge
dynamics of edge position
Oceanography
GC1-1581
spellingShingle Arctic
sea ice
sea ice edge
dynamics of edge position
Oceanography
GC1-1581
A.E. Bukatov
A.A. Bukatov
M.V. Babii
Response of Influence of Internal and External Factors in the Latitudinal Sea Ice Edge Displacement in the Arctic Basin
topic_facet Arctic
sea ice
sea ice edge
dynamics of edge position
Oceanography
GC1-1581
description Inter-annual climatic response of the sea ice edge latitudinal displacement in the Arctic to variability of the large-scale atmospheric circulation (the Arctic Oscillation and North Atlantic Oscillation), location of the Gulf Stream northern boundary and solar activity in 1969–2012 is studied. It is noted that the most significant ice edge latitudinal displacements in the intra-annual cycle were observed westward of Novaya Zemlya and in the Bering Strait area. It is shown that, depending on the longitudinal sector, response of the edge geographical position to changes of the atmospheric circulation and the Gulf Stream indices can be manifested both quasi-synchronously and with a delay. Exceptions are the Greenland Sea and the Norwegian Sea areas as well as the Barents Sea western part where ice edge displacements advance the Gulf Stream index variation. The correlation between the edge latitudinal displacement along its perimeter and the Wolf numbers variation is assessed. It is received that the oscillations of cross-correlation functions with a period which is close to 11-year one (Schwabe Cycle) are observed on each longitude at that. In the variations of cross-correlation functions from their average position, solar activity variation is manifested in the edge position displacement with up to two-year delay.
format Article in Journal/Newspaper
author A.E. Bukatov
A.A. Bukatov
M.V. Babii
author_facet A.E. Bukatov
A.A. Bukatov
M.V. Babii
author_sort A.E. Bukatov
title Response of Influence of Internal and External Factors in the Latitudinal Sea Ice Edge Displacement in the Arctic Basin
title_short Response of Influence of Internal and External Factors in the Latitudinal Sea Ice Edge Displacement in the Arctic Basin
title_full Response of Influence of Internal and External Factors in the Latitudinal Sea Ice Edge Displacement in the Arctic Basin
title_fullStr Response of Influence of Internal and External Factors in the Latitudinal Sea Ice Edge Displacement in the Arctic Basin
title_full_unstemmed Response of Influence of Internal and External Factors in the Latitudinal Sea Ice Edge Displacement in the Arctic Basin
title_sort response of influence of internal and external factors in the latitudinal sea ice edge displacement in the arctic basin
publisher Federal State Budget Scientific Institution «Marine Hydrophysical Institute of RAS»
publishDate 2016
url https://doi.org/10.22449/1573-160X-2016-6-24-31
https://doaj.org/article/6f431410e383499590f44bedcaf29fbf
geographic Arctic
Barents Sea
Bering Strait
Greenland
Norwegian Sea
geographic_facet Arctic
Barents Sea
Bering Strait
Greenland
Norwegian Sea
genre Arctic Basin
Arctic
Barents Sea
Bering Strait
Greenland
Greenland Sea
North Atlantic
North Atlantic oscillation
Norwegian Sea
Novaya Zemlya
Sea ice
genre_facet Arctic Basin
Arctic
Barents Sea
Bering Strait
Greenland
Greenland Sea
North Atlantic
North Atlantic oscillation
Norwegian Sea
Novaya Zemlya
Sea ice
op_source Physical Oceanography, Iss 6, Pp 24-31 (2016)
op_relation http://physical-oceanography.ru/repository/2016/6/en_201606_03.pdf
https://doaj.org/toc/1573-160X
doi:10.22449/1573-160X-2016-6-24-31
1573-160X
https://doaj.org/article/6f431410e383499590f44bedcaf29fbf
op_doi https://doi.org/10.22449/1573-160X-2016-6-24-31
container_title Physical Oceanography
container_issue 6
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