Fluctuations and seasonality in the Arctic sea ice area: A sudden regime shift in 2007?

Since the beginning of satellite observations, the Arctic sea ice extent has shown a downward trend. The decline has been weaker in the March maximum than in the September minimum and masked by inter-annual fluctuations. One of the less understood aspects of the sea ice response is the persistence t...

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Main Authors: Ditlevsen, Peter D., Cvijanovic, Ivana
Format: Report
Language:unknown
Published: arXiv 2013
Subjects:
Online Access:https://dx.doi.org/10.48550/arxiv.1308.4821
https://arxiv.org/abs/1308.4821
id ftdatacite:10.48550/arxiv.1308.4821
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spelling ftdatacite:10.48550/arxiv.1308.4821 2023-05-15T14:55:51+02:00 Fluctuations and seasonality in the Arctic sea ice area: A sudden regime shift in 2007? Ditlevsen, Peter D. Cvijanovic, Ivana 2013 https://dx.doi.org/10.48550/arxiv.1308.4821 https://arxiv.org/abs/1308.4821 unknown arXiv arXiv.org perpetual, non-exclusive license http://arxiv.org/licenses/nonexclusive-distrib/1.0/ Atmospheric and Oceanic Physics physics.ao-ph Chaotic Dynamics nlin.CD Data Analysis, Statistics and Probability physics.data-an FOS Physical sciences Preprint Article article CreativeWork 2013 ftdatacite https://doi.org/10.48550/arxiv.1308.4821 2022-04-01T13:12:47Z Since the beginning of satellite observations, the Arctic sea ice extent has shown a downward trend. The decline has been weaker in the March maximum than in the September minimum and masked by inter-annual fluctuations. One of the less understood aspects of the sea ice response is the persistence times for fluctuations, which could indicate the dominant physical processes behind the sea ice decline. To determine the fluctuation persistence times, however, it is necessary to first filter out the dominant effect of the seasonal cycle. In the current study, we thus develop a statistical model, which accurately decomposes the ice area changes into: (1) a variable seasonal cycle component with a constant shape and (2) a residual (short term) fluctuation. We find the persistence time of fluctuations to be only about three weeks, independently from season, which is substantially shorter than previously reported. Such short time scale points to the dominance of atmospheric forcing. The shape of the seasonal cycle is surprisingly constant for the whole observational record despite the rapid decline. This is in agreement with the suggestion that the asymmetry of the seasonal cycle is an effect of Arctic land-sea geography, which has not changed with climate change. The analysis suggest a jump in the annual sea ice area amplitude occurring in 2007, from which it has not yet recovered, possibly revealing a permanent amplitude shift. In physical sense, this could imply a shift towards the younger, thinner and more susceptible ice cover commencing after the immense 2007 multi-year ice loss. : 8 pages, 4 figures Report Arctic Climate change Sea ice DataCite Metadata Store (German National Library of Science and Technology) Arctic
institution Open Polar
collection DataCite Metadata Store (German National Library of Science and Technology)
op_collection_id ftdatacite
language unknown
topic Atmospheric and Oceanic Physics physics.ao-ph
Chaotic Dynamics nlin.CD
Data Analysis, Statistics and Probability physics.data-an
FOS Physical sciences
spellingShingle Atmospheric and Oceanic Physics physics.ao-ph
Chaotic Dynamics nlin.CD
Data Analysis, Statistics and Probability physics.data-an
FOS Physical sciences
Ditlevsen, Peter D.
Cvijanovic, Ivana
Fluctuations and seasonality in the Arctic sea ice area: A sudden regime shift in 2007?
topic_facet Atmospheric and Oceanic Physics physics.ao-ph
Chaotic Dynamics nlin.CD
Data Analysis, Statistics and Probability physics.data-an
FOS Physical sciences
description Since the beginning of satellite observations, the Arctic sea ice extent has shown a downward trend. The decline has been weaker in the March maximum than in the September minimum and masked by inter-annual fluctuations. One of the less understood aspects of the sea ice response is the persistence times for fluctuations, which could indicate the dominant physical processes behind the sea ice decline. To determine the fluctuation persistence times, however, it is necessary to first filter out the dominant effect of the seasonal cycle. In the current study, we thus develop a statistical model, which accurately decomposes the ice area changes into: (1) a variable seasonal cycle component with a constant shape and (2) a residual (short term) fluctuation. We find the persistence time of fluctuations to be only about three weeks, independently from season, which is substantially shorter than previously reported. Such short time scale points to the dominance of atmospheric forcing. The shape of the seasonal cycle is surprisingly constant for the whole observational record despite the rapid decline. This is in agreement with the suggestion that the asymmetry of the seasonal cycle is an effect of Arctic land-sea geography, which has not changed with climate change. The analysis suggest a jump in the annual sea ice area amplitude occurring in 2007, from which it has not yet recovered, possibly revealing a permanent amplitude shift. In physical sense, this could imply a shift towards the younger, thinner and more susceptible ice cover commencing after the immense 2007 multi-year ice loss. : 8 pages, 4 figures
format Report
author Ditlevsen, Peter D.
Cvijanovic, Ivana
author_facet Ditlevsen, Peter D.
Cvijanovic, Ivana
author_sort Ditlevsen, Peter D.
title Fluctuations and seasonality in the Arctic sea ice area: A sudden regime shift in 2007?
title_short Fluctuations and seasonality in the Arctic sea ice area: A sudden regime shift in 2007?
title_full Fluctuations and seasonality in the Arctic sea ice area: A sudden regime shift in 2007?
title_fullStr Fluctuations and seasonality in the Arctic sea ice area: A sudden regime shift in 2007?
title_full_unstemmed Fluctuations and seasonality in the Arctic sea ice area: A sudden regime shift in 2007?
title_sort fluctuations and seasonality in the arctic sea ice area: a sudden regime shift in 2007?
publisher arXiv
publishDate 2013
url https://dx.doi.org/10.48550/arxiv.1308.4821
https://arxiv.org/abs/1308.4821
geographic Arctic
geographic_facet Arctic
genre Arctic
Climate change
Sea ice
genre_facet Arctic
Climate change
Sea ice
op_rights arXiv.org perpetual, non-exclusive license
http://arxiv.org/licenses/nonexclusive-distrib/1.0/
op_doi https://doi.org/10.48550/arxiv.1308.4821
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