GLOBAL CHANGES IN THE SEA ICE COVER AND ASSOCIATED SURFACE TEMPERATURE CHANGES

The trends in the sea ice cover in the two hemispheres have been observed to be asymmetric with the rate of change in the Arctic being negative at −3.8 % per decade while that of the Antarctic is positive at 1.7 % per decade. These observations are confirmed in this study through analyses of a more...

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Published in:The International Archives of the Photogrammetry, Remote Sensing and Spatial Information Sciences
Main Author: Comiso, Josefino C.
Format: Text
Language:English
Published: 2018
Subjects:
Online Access:https://doi.org/10.5194/isprs-archives-XLI-B8-469-2016
https://www.int-arch-photogramm-remote-sens-spatial-inf-sci.net/XLI-B8/469/2016/
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spelling ftcopernicus:oai:publications.copernicus.org:isprs-archives53283 2023-05-15T13:43:09+02:00 GLOBAL CHANGES IN THE SEA ICE COVER AND ASSOCIATED SURFACE TEMPERATURE CHANGES Comiso, Josefino C. 2018-01-15 application/pdf https://doi.org/10.5194/isprs-archives-XLI-B8-469-2016 https://www.int-arch-photogramm-remote-sens-spatial-inf-sci.net/XLI-B8/469/2016/ eng eng doi:10.5194/isprs-archives-XLI-B8-469-2016 https://www.int-arch-photogramm-remote-sens-spatial-inf-sci.net/XLI-B8/469/2016/ eISSN: 2194-9034 Text 2018 ftcopernicus https://doi.org/10.5194/isprs-archives-XLI-B8-469-2016 2019-12-24T09:52:11Z The trends in the sea ice cover in the two hemispheres have been observed to be asymmetric with the rate of change in the Arctic being negative at −3.8 % per decade while that of the Antarctic is positive at 1.7 % per decade. These observations are confirmed in this study through analyses of a more robust data set that has been enhanced for better consistency and updated for improved statistics. With reports of anthropogenic global warming such phenomenon appears physically counter intuitive but trend studies of surface temperature over the same time period show the occurrence of a similar asymmetry. Satellite surface temperature data show that while global warming is strong and dominant in the Arctic, it is relatively minor in the Antarctic with the trends in sea ice covered areas and surrounding ice free regions observed to be even negative. A strong correlation of ice extent with surface temperature is observed, especially during the growth season, and the observed trends in the sea ice cover are coherent with the trends in surface temperature. The trend of global averages of the ice cover is negative but modest and is consistent and compatible with the positive but modest trend in global surface temperature. A continuation of the trend would mean the disappearance of summer ice by the end of the century but modelling projections indicate that the summer ice could be salvaged if anthropogenic greenhouse gases in the atmosphere are kept constant at the current level. Text Antarc* Antarctic Arctic Global warming Sea ice ice covered areas Copernicus Publications: E-Journals Antarctic Arctic The Antarctic The International Archives of the Photogrammetry, Remote Sensing and Spatial Information Sciences XLI-B8 469 479
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collection Copernicus Publications: E-Journals
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language English
description The trends in the sea ice cover in the two hemispheres have been observed to be asymmetric with the rate of change in the Arctic being negative at −3.8 % per decade while that of the Antarctic is positive at 1.7 % per decade. These observations are confirmed in this study through analyses of a more robust data set that has been enhanced for better consistency and updated for improved statistics. With reports of anthropogenic global warming such phenomenon appears physically counter intuitive but trend studies of surface temperature over the same time period show the occurrence of a similar asymmetry. Satellite surface temperature data show that while global warming is strong and dominant in the Arctic, it is relatively minor in the Antarctic with the trends in sea ice covered areas and surrounding ice free regions observed to be even negative. A strong correlation of ice extent with surface temperature is observed, especially during the growth season, and the observed trends in the sea ice cover are coherent with the trends in surface temperature. The trend of global averages of the ice cover is negative but modest and is consistent and compatible with the positive but modest trend in global surface temperature. A continuation of the trend would mean the disappearance of summer ice by the end of the century but modelling projections indicate that the summer ice could be salvaged if anthropogenic greenhouse gases in the atmosphere are kept constant at the current level.
format Text
author Comiso, Josefino C.
spellingShingle Comiso, Josefino C.
GLOBAL CHANGES IN THE SEA ICE COVER AND ASSOCIATED SURFACE TEMPERATURE CHANGES
author_facet Comiso, Josefino C.
author_sort Comiso, Josefino C.
title GLOBAL CHANGES IN THE SEA ICE COVER AND ASSOCIATED SURFACE TEMPERATURE CHANGES
title_short GLOBAL CHANGES IN THE SEA ICE COVER AND ASSOCIATED SURFACE TEMPERATURE CHANGES
title_full GLOBAL CHANGES IN THE SEA ICE COVER AND ASSOCIATED SURFACE TEMPERATURE CHANGES
title_fullStr GLOBAL CHANGES IN THE SEA ICE COVER AND ASSOCIATED SURFACE TEMPERATURE CHANGES
title_full_unstemmed GLOBAL CHANGES IN THE SEA ICE COVER AND ASSOCIATED SURFACE TEMPERATURE CHANGES
title_sort global changes in the sea ice cover and associated surface temperature changes
publishDate 2018
url https://doi.org/10.5194/isprs-archives-XLI-B8-469-2016
https://www.int-arch-photogramm-remote-sens-spatial-inf-sci.net/XLI-B8/469/2016/
geographic Antarctic
Arctic
The Antarctic
geographic_facet Antarctic
Arctic
The Antarctic
genre Antarc*
Antarctic
Arctic
Global warming
Sea ice
ice covered areas
genre_facet Antarc*
Antarctic
Arctic
Global warming
Sea ice
ice covered areas
op_source eISSN: 2194-9034
op_relation doi:10.5194/isprs-archives-XLI-B8-469-2016
https://www.int-arch-photogramm-remote-sens-spatial-inf-sci.net/XLI-B8/469/2016/
op_doi https://doi.org/10.5194/isprs-archives-XLI-B8-469-2016
container_title The International Archives of the Photogrammetry, Remote Sensing and Spatial Information Sciences
container_volume XLI-B8
container_start_page 469
op_container_end_page 479
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