Time varying arctic climate change amplification
During the past 130 years the global mean surface air temperature has risen by about 0.75 K. Due to feedbacks -- including the snow/ice albedo feedback -- the warming in the Arctic is expected to proceed at a faster rate than the global average. Climate model simulations suggest that this Arctic amp...
Main Authors: | , , , |
---|---|
Other Authors: | |
Format: | Article in Journal/Newspaper |
Language: | English |
Published: |
Los Alamos National Laboratory
2009
|
Subjects: | |
Online Access: | https://digital.library.unt.edu/ark:/67531/metadc926903/ |
id |
ftunivnotexas:info:ark/67531/metadc926903 |
---|---|
record_format |
openpolar |
spelling |
ftunivnotexas:info:ark/67531/metadc926903 2023-05-15T13:10:28+02:00 Time varying arctic climate change amplification Chylek, P. Dubey, M. K. Lesins, G. Wang, M. United States. Department of Energy. 2009-01-01 Text https://digital.library.unt.edu/ark:/67531/metadc926903/ English eng Los Alamos National Laboratory rep-no: LA-UR-09-01197 rep-no: LA-UR-09-1197 grantno: AC52-06NA25396 osti: 956565 https://digital.library.unt.edu/ark:/67531/metadc926903/ ark: ark:/67531/metadc926903 Journal Name: Geophysical Research Letters Amplification Greenland Seas 58 Albedo Ambient Temperature Melting Climates Time Dependence Ice Arctic Regions Climate Models Surface Air Article 2009 ftunivnotexas 2022-04-16T22:08:13Z During the past 130 years the global mean surface air temperature has risen by about 0.75 K. Due to feedbacks -- including the snow/ice albedo feedback -- the warming in the Arctic is expected to proceed at a faster rate than the global average. Climate model simulations suggest that this Arctic amplification produces warming that is two to three times larger than the global mean. Understanding the Arctic amplification is essential for projections of future Arctic climate including sea ice extent and melting of the Greenland ice sheet. We use the temperature records from the Arctic stations to show that (a) the Arctic amplification is larger at latitudes above 700 N compared to those within 64-70oN belt, and that, surprisingly; (b) the ratio of the Arctic to global rate of temperature change is not constant but varies on the decadal timescale. This time dependence will affect future projections of climate changes in the Arctic. Article in Journal/Newspaper albedo Arctic Climate change Greenland Ice Sheet Sea ice University of North Texas: UNT Digital Library Arctic Greenland |
institution |
Open Polar |
collection |
University of North Texas: UNT Digital Library |
op_collection_id |
ftunivnotexas |
language |
English |
topic |
Amplification Greenland Seas 58 Albedo Ambient Temperature Melting Climates Time Dependence Ice Arctic Regions Climate Models Surface Air |
spellingShingle |
Amplification Greenland Seas 58 Albedo Ambient Temperature Melting Climates Time Dependence Ice Arctic Regions Climate Models Surface Air Chylek, P. Dubey, M. K. Lesins, G. Wang, M. Time varying arctic climate change amplification |
topic_facet |
Amplification Greenland Seas 58 Albedo Ambient Temperature Melting Climates Time Dependence Ice Arctic Regions Climate Models Surface Air |
description |
During the past 130 years the global mean surface air temperature has risen by about 0.75 K. Due to feedbacks -- including the snow/ice albedo feedback -- the warming in the Arctic is expected to proceed at a faster rate than the global average. Climate model simulations suggest that this Arctic amplification produces warming that is two to three times larger than the global mean. Understanding the Arctic amplification is essential for projections of future Arctic climate including sea ice extent and melting of the Greenland ice sheet. We use the temperature records from the Arctic stations to show that (a) the Arctic amplification is larger at latitudes above 700 N compared to those within 64-70oN belt, and that, surprisingly; (b) the ratio of the Arctic to global rate of temperature change is not constant but varies on the decadal timescale. This time dependence will affect future projections of climate changes in the Arctic. |
author2 |
United States. Department of Energy. |
format |
Article in Journal/Newspaper |
author |
Chylek, P. Dubey, M. K. Lesins, G. Wang, M. |
author_facet |
Chylek, P. Dubey, M. K. Lesins, G. Wang, M. |
author_sort |
Chylek, P. |
title |
Time varying arctic climate change amplification |
title_short |
Time varying arctic climate change amplification |
title_full |
Time varying arctic climate change amplification |
title_fullStr |
Time varying arctic climate change amplification |
title_full_unstemmed |
Time varying arctic climate change amplification |
title_sort |
time varying arctic climate change amplification |
publisher |
Los Alamos National Laboratory |
publishDate |
2009 |
url |
https://digital.library.unt.edu/ark:/67531/metadc926903/ |
geographic |
Arctic Greenland |
geographic_facet |
Arctic Greenland |
genre |
albedo Arctic Climate change Greenland Ice Sheet Sea ice |
genre_facet |
albedo Arctic Climate change Greenland Ice Sheet Sea ice |
op_source |
Journal Name: Geophysical Research Letters |
op_relation |
rep-no: LA-UR-09-01197 rep-no: LA-UR-09-1197 grantno: AC52-06NA25396 osti: 956565 https://digital.library.unt.edu/ark:/67531/metadc926903/ ark: ark:/67531/metadc926903 |
_version_ |
1766230685148774400 |