Global Warming and Changes in

This paper presents a statistical analysis of sea ice in the Greenland Sea (70-80N and 10W-10E) from January 1979 to December 2007. We define four variables from satellite images: ice extent, ice area, eastward ice extent at 75N, and the shape of the ice edge. We establish relationships between thes...

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Main Authors: Sea Ice In The Greenl, Maxine Von Eye, Alexander Von Eye
Other Authors: The Pennsylvania State University CiteSeerX Archives
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Language:English
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Online Access:http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.501.9905
http://interstat.statjournals.net/YEAR/2009/articles/0905003.pdf
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spelling ftciteseerx:oai:CiteSeerX.psu:10.1.1.501.9905 2023-05-15T15:08:30+02:00 Global Warming and Changes in Sea Ice In The Greenl Maxine Von Eye Alexander Von Eye The Pennsylvania State University CiteSeerX Archives application/pdf http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.501.9905 http://interstat.statjournals.net/YEAR/2009/articles/0905003.pdf en eng http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.501.9905 http://interstat.statjournals.net/YEAR/2009/articles/0905003.pdf Metadata may be used without restrictions as long as the oai identifier remains attached to it. http://interstat.statjournals.net/YEAR/2009/articles/0905003.pdf text ftciteseerx 2016-01-08T09:10:59Z This paper presents a statistical analysis of sea ice in the Greenland Sea (70-80N and 10W-10E) from January 1979 to December 2007. We define four variables from satellite images: ice extent, ice area, eastward ice extent at 75N, and the shape of the ice edge. We establish relationships between these ice variables and five climate variables: sea surface temperature (SST), air temperature at Jan Mayen Island (JM), sea surface pressure (SSP), North Atlantic Oscillation (NAO) and Arctic Oscillation (AO). The ice extent, ice area and eastward ice extent are highly correlated with SST and JM over the whole time period, while SSP, NAO and AO are only correlated with the ice variables over shorter (one year) periods. When considering the different shapes of the ice edge, an ANOVA model shows that 49 % of the variance in extent can be explained by the shape of the ice edge, and similar amounts for the eastward ice extent and ice area. Fourier analysis of the sea ice data shows a 10 year peak which is consistent with previous hypotheses in work done on the Greenland Sea. Finally, we show that the negative trend in the sea ice extent, ice area and eastward extent is statistically significant. This can be interpreted as yet another indicator of the global warming that has been taking place for the last 30 years. 1 von Eye, et al Sea Ice in the Greenland Sea Text Arctic Global warming Greenland Greenland Sea Jan Mayen Jan Mayen Island North Atlantic North Atlantic oscillation Sea ice Unknown Arctic Greenland Jan Mayen
institution Open Polar
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description This paper presents a statistical analysis of sea ice in the Greenland Sea (70-80N and 10W-10E) from January 1979 to December 2007. We define four variables from satellite images: ice extent, ice area, eastward ice extent at 75N, and the shape of the ice edge. We establish relationships between these ice variables and five climate variables: sea surface temperature (SST), air temperature at Jan Mayen Island (JM), sea surface pressure (SSP), North Atlantic Oscillation (NAO) and Arctic Oscillation (AO). The ice extent, ice area and eastward ice extent are highly correlated with SST and JM over the whole time period, while SSP, NAO and AO are only correlated with the ice variables over shorter (one year) periods. When considering the different shapes of the ice edge, an ANOVA model shows that 49 % of the variance in extent can be explained by the shape of the ice edge, and similar amounts for the eastward ice extent and ice area. Fourier analysis of the sea ice data shows a 10 year peak which is consistent with previous hypotheses in work done on the Greenland Sea. Finally, we show that the negative trend in the sea ice extent, ice area and eastward extent is statistically significant. This can be interpreted as yet another indicator of the global warming that has been taking place for the last 30 years. 1 von Eye, et al Sea Ice in the Greenland Sea
author2 The Pennsylvania State University CiteSeerX Archives
format Text
author Sea Ice In The Greenl
Maxine Von Eye
Alexander Von Eye
spellingShingle Sea Ice In The Greenl
Maxine Von Eye
Alexander Von Eye
Global Warming and Changes in
author_facet Sea Ice In The Greenl
Maxine Von Eye
Alexander Von Eye
author_sort Sea Ice In The Greenl
title Global Warming and Changes in
title_short Global Warming and Changes in
title_full Global Warming and Changes in
title_fullStr Global Warming and Changes in
title_full_unstemmed Global Warming and Changes in
title_sort global warming and changes in
url http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.501.9905
http://interstat.statjournals.net/YEAR/2009/articles/0905003.pdf
geographic Arctic
Greenland
Jan Mayen
geographic_facet Arctic
Greenland
Jan Mayen
genre Arctic
Global warming
Greenland
Greenland Sea
Jan Mayen
Jan Mayen Island
North Atlantic
North Atlantic oscillation
Sea ice
genre_facet Arctic
Global warming
Greenland
Greenland Sea
Jan Mayen
Jan Mayen Island
North Atlantic
North Atlantic oscillation
Sea ice
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