Modeling the annual cycle of daily Antarctic sea ice extent

The total Antarctic sea ice extent (SIE) experiences a distinct annual cycle, peaking in September and reaching its minimum in February. In this paper we propose a mathematical and statistical decomposition of this temporal variation in SIE. Each component is interpretable and, when combined, gives...

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Main Authors: Handcock, Mark S, Raphael, Marilyn N
Format: Article in Journal/Newspaper
Language:unknown
Published: eScholarship, University of California 2020
Subjects:
Online Access:https://escholarship.org/uc/item/5jh7s9wg
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spelling ftcdlib:oai:escholarship.org:ark:/13030/qt5jh7s9wg 2023-11-05T03:36:48+01:00 Modeling the annual cycle of daily Antarctic sea ice extent Handcock, Mark S Raphael, Marilyn N 2159 - 2172 2020-01-01 application/pdf https://escholarship.org/uc/item/5jh7s9wg unknown eScholarship, University of California qt5jh7s9wg https://escholarship.org/uc/item/5jh7s9wg public The Cryosphere, vol 14, iss 7 Earth Sciences Oceanography Physical Geography and Environmental Geoscience Meteorology & Atmospheric Sciences article 2020 ftcdlib 2023-10-09T18:05:56Z The total Antarctic sea ice extent (SIE) experiences a distinct annual cycle, peaking in September and reaching its minimum in February. In this paper we propose a mathematical and statistical decomposition of this temporal variation in SIE. Each component is interpretable and, when combined, gives a complete picture of the variation in the sea ice. We consider timescales varying from the instantaneous and not previously defined to the multi-decadal curvilinear trend, the longest. Because our representation is daily, these timescales of variability give precise information about the timing and rates of advance and retreat of the ice and may be used to diagnose physical contributors to variability in the sea ice. We define a number of annual cycles each capturing different components of variation, especially the yearly amplitude and phase that are major contributors to SIE variation. Using daily sea ice concentration data, we show that our proposed invariant annual cycle explains 29% more of the variation in daily SIE than the traditional method. The proposed annual cycle that incorporates amplitude and phase variation explains 77% more variation than the traditional method. The variation in phase explains more of the variability in SIE than the amplitude. Using our methodology, we show that the anomalous decay of sea ice in 2016 was associated largely with a change of phase rather than amplitude. We show that the long term trend in Antarctic sea ice extent is strongly curvilinear and the reported positive linear trend is small and dependent strongly on a positive trend that began around 2011 and continued until 2016. Article in Journal/Newspaper Antarc* Antarctic Sea ice The Cryosphere University of California: eScholarship
institution Open Polar
collection University of California: eScholarship
op_collection_id ftcdlib
language unknown
topic Earth Sciences
Oceanography
Physical Geography and Environmental Geoscience
Meteorology & Atmospheric Sciences
spellingShingle Earth Sciences
Oceanography
Physical Geography and Environmental Geoscience
Meteorology & Atmospheric Sciences
Handcock, Mark S
Raphael, Marilyn N
Modeling the annual cycle of daily Antarctic sea ice extent
topic_facet Earth Sciences
Oceanography
Physical Geography and Environmental Geoscience
Meteorology & Atmospheric Sciences
description The total Antarctic sea ice extent (SIE) experiences a distinct annual cycle, peaking in September and reaching its minimum in February. In this paper we propose a mathematical and statistical decomposition of this temporal variation in SIE. Each component is interpretable and, when combined, gives a complete picture of the variation in the sea ice. We consider timescales varying from the instantaneous and not previously defined to the multi-decadal curvilinear trend, the longest. Because our representation is daily, these timescales of variability give precise information about the timing and rates of advance and retreat of the ice and may be used to diagnose physical contributors to variability in the sea ice. We define a number of annual cycles each capturing different components of variation, especially the yearly amplitude and phase that are major contributors to SIE variation. Using daily sea ice concentration data, we show that our proposed invariant annual cycle explains 29% more of the variation in daily SIE than the traditional method. The proposed annual cycle that incorporates amplitude and phase variation explains 77% more variation than the traditional method. The variation in phase explains more of the variability in SIE than the amplitude. Using our methodology, we show that the anomalous decay of sea ice in 2016 was associated largely with a change of phase rather than amplitude. We show that the long term trend in Antarctic sea ice extent is strongly curvilinear and the reported positive linear trend is small and dependent strongly on a positive trend that began around 2011 and continued until 2016.
format Article in Journal/Newspaper
author Handcock, Mark S
Raphael, Marilyn N
author_facet Handcock, Mark S
Raphael, Marilyn N
author_sort Handcock, Mark S
title Modeling the annual cycle of daily Antarctic sea ice extent
title_short Modeling the annual cycle of daily Antarctic sea ice extent
title_full Modeling the annual cycle of daily Antarctic sea ice extent
title_fullStr Modeling the annual cycle of daily Antarctic sea ice extent
title_full_unstemmed Modeling the annual cycle of daily Antarctic sea ice extent
title_sort modeling the annual cycle of daily antarctic sea ice extent
publisher eScholarship, University of California
publishDate 2020
url https://escholarship.org/uc/item/5jh7s9wg
op_coverage 2159 - 2172
genre Antarc*
Antarctic
Sea ice
The Cryosphere
genre_facet Antarc*
Antarctic
Sea ice
The Cryosphere
op_source The Cryosphere, vol 14, iss 7
op_relation qt5jh7s9wg
https://escholarship.org/uc/item/5jh7s9wg
op_rights public
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