Climatic change on King George Island in the years 1948–2011

Abstract The climatic change on King George Island (KGI) in the South Shetland Islands, Antarctica, in the years of 1948-2011 are presented. In the reference period, a statistically significant increase in the air temperature (0.19ºC/10 years, 1.2ºC in the analysed period) occurred along with a decr...

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Published in:Polish Polar Research
Main Authors: Kejna, Marek, Araźny, Andrzej, Sobota, Ireneusz
Format: Article in Journal/Newspaper
Language:unknown
Published: Walter de Gruyter GmbH 2013
Subjects:
Online Access:http://dx.doi.org/10.2478/popore-2013-0004
http://content.sciendo.com/view/journals/popore/34/2/article-p213.xml
https://www.degruyter.com/view/j/popore.2013.34.issue-2/popore-2013-0004/popore-2013-0004.pdf
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spelling crdegruyter:10.2478/popore-2013-0004 2023-05-15T14:12:18+02:00 Climatic change on King George Island in the years 1948–2011 Kejna, Marek Araźny, Andrzej Sobota, Ireneusz 2013 http://dx.doi.org/10.2478/popore-2013-0004 http://content.sciendo.com/view/journals/popore/34/2/article-p213.xml https://www.degruyter.com/view/j/popore.2013.34.issue-2/popore-2013-0004/popore-2013-0004.pdf unknown Walter de Gruyter GmbH Polish Polar Research volume 34, issue 2, page 213-235 ISSN 2081-8262 0138-0338 Ecology Ecology, Evolution, Behavior and Systematics journal-article 2013 crdegruyter https://doi.org/10.2478/popore-2013-0004 2022-07-08T14:12:08Z Abstract The climatic change on King George Island (KGI) in the South Shetland Islands, Antarctica, in the years of 1948-2011 are presented. In the reference period, a statistically significant increase in the air temperature (0.19ºC/10 years, 1.2ºC in the analysed period) occurred along with a decrease in atmospheric pressure (−0.36 hPa/10 years, 2.3 hPa). In winter time, the warming up is more than twice as large as in summer. This leads to decrease in the amplitude of the annual cycle of air temperature. On KGI, there is also a warming trend of daily maximum and daily minimum air temperature. The evidently faster increase in daily minimum results in a decrease of the diurnal temperature range. The largest changes of air pressure took place in the summertime (−0.58 hPa/10 years) and winter (−0.34 hPa/10 years). The Semiannual Oscillation pattern of air pressure was disturbed. Climate changes on KGI are correlated with changing surface temperatures of the ocean and the concentra− tion of sea ice. The precipitation on KGI is characterised by substantial variability year to year. In the analysed period, no statistically significant trend in atmospheric precipitation can be observed. The climate change on KGI results in substantial and rapid changes in the environment, which poses a great threat to the local ecosystem. Article in Journal/Newspaper Antarc* Antarctica King George Island Polar Research Sea ice South Shetland Islands De Gruyter (via Crossref) King George Island South Shetland Islands Polish Polar Research 34 2 213 235
institution Open Polar
collection De Gruyter (via Crossref)
op_collection_id crdegruyter
language unknown
topic Ecology
Ecology, Evolution, Behavior and Systematics
spellingShingle Ecology
Ecology, Evolution, Behavior and Systematics
Kejna, Marek
Araźny, Andrzej
Sobota, Ireneusz
Climatic change on King George Island in the years 1948–2011
topic_facet Ecology
Ecology, Evolution, Behavior and Systematics
description Abstract The climatic change on King George Island (KGI) in the South Shetland Islands, Antarctica, in the years of 1948-2011 are presented. In the reference period, a statistically significant increase in the air temperature (0.19ºC/10 years, 1.2ºC in the analysed period) occurred along with a decrease in atmospheric pressure (−0.36 hPa/10 years, 2.3 hPa). In winter time, the warming up is more than twice as large as in summer. This leads to decrease in the amplitude of the annual cycle of air temperature. On KGI, there is also a warming trend of daily maximum and daily minimum air temperature. The evidently faster increase in daily minimum results in a decrease of the diurnal temperature range. The largest changes of air pressure took place in the summertime (−0.58 hPa/10 years) and winter (−0.34 hPa/10 years). The Semiannual Oscillation pattern of air pressure was disturbed. Climate changes on KGI are correlated with changing surface temperatures of the ocean and the concentra− tion of sea ice. The precipitation on KGI is characterised by substantial variability year to year. In the analysed period, no statistically significant trend in atmospheric precipitation can be observed. The climate change on KGI results in substantial and rapid changes in the environment, which poses a great threat to the local ecosystem.
format Article in Journal/Newspaper
author Kejna, Marek
Araźny, Andrzej
Sobota, Ireneusz
author_facet Kejna, Marek
Araźny, Andrzej
Sobota, Ireneusz
author_sort Kejna, Marek
title Climatic change on King George Island in the years 1948–2011
title_short Climatic change on King George Island in the years 1948–2011
title_full Climatic change on King George Island in the years 1948–2011
title_fullStr Climatic change on King George Island in the years 1948–2011
title_full_unstemmed Climatic change on King George Island in the years 1948–2011
title_sort climatic change on king george island in the years 1948–2011
publisher Walter de Gruyter GmbH
publishDate 2013
url http://dx.doi.org/10.2478/popore-2013-0004
http://content.sciendo.com/view/journals/popore/34/2/article-p213.xml
https://www.degruyter.com/view/j/popore.2013.34.issue-2/popore-2013-0004/popore-2013-0004.pdf
geographic King George Island
South Shetland Islands
geographic_facet King George Island
South Shetland Islands
genre Antarc*
Antarctica
King George Island
Polar Research
Sea ice
South Shetland Islands
genre_facet Antarc*
Antarctica
King George Island
Polar Research
Sea ice
South Shetland Islands
op_source Polish Polar Research
volume 34, issue 2, page 213-235
ISSN 2081-8262 0138-0338
op_doi https://doi.org/10.2478/popore-2013-0004
container_title Polish Polar Research
container_volume 34
container_issue 2
container_start_page 213
op_container_end_page 235
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