Recent climate trends

In concert with the rest of the world, the climate of Antarctica is changing. This change is seen in keyclimate parameters, such as the atmospheric circulation, surface air temperature, precipitation, sea iceextent, and the temperature of the Southern Ocean. Surface air temperatures are increasing,...

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Main Authors: Raphael, MN, Hobbs, WR, Marshall, GJ, Stammerjohn, SE
Format: Book Part
Language:English
Published: Academic Press 2020
Subjects:
Online Access:https://www.sciencedirect.com/science/article/pii/B9780128179253000136?via%3Dihub
https://doi.org/10.1016/B978-0-12-817925-3.00013-6
http://ecite.utas.edu.au/145274
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spelling ftunivtasecite:oai:ecite.utas.edu.au:145274 2023-05-15T13:42:41+02:00 Recent climate trends Raphael, MN Hobbs, WR Marshall, GJ Stammerjohn, SE 2020 https://www.sciencedirect.com/science/article/pii/B9780128179253000136?via%3Dihub https://doi.org/10.1016/B978-0-12-817925-3.00013-6 http://ecite.utas.edu.au/145274 en eng Academic Press http://dx.doi.org/10.1016/B978-0-12-817925-3.00013-6 Raphael, MN and Hobbs, WR and Marshall, GJ and Stammerjohn, SE, Recent climate trends, Past Antarctica: Paleoclimatology and Climate Change, Academic Press, M Oliva and J Ruiz-Fernandez (ed), United Kingdom, pp. 241-257. ISBN 9780128179253 (2020) [Research Book Chapter] 9780128179253 http://ecite.utas.edu.au/145274 Earth Sciences Climate change science Climatology Research Book Chapter NonPeerReviewed 2020 ftunivtasecite https://doi.org/10.1016/B978-0-12-817925-3.00013-6 2022-12-26T23:17:08Z In concert with the rest of the world, the climate of Antarctica is changing. This change is seen in keyclimate parameters, such as the atmospheric circulation, surface air temperature, precipitation, sea iceextent, and the temperature of the Southern Ocean. Surface air temperatures are increasing, and indeedfor the second half of the 20th century, the temperature increase on the Antarctic Peninsula was amongthe largest experienced on Earth (Steig et al., 2009). Total sea ice extent is not decreasing, as is occurringin the Arctic, but the deeper levels of the Southern Ocean are warming, similar to most otheroceans. The changes are not uniform in time or space and are due to remote and proximate influences.This chapter discusses the changes in climate at the surface and the deep ocean, including the role thatthe leading atmospheric circulation modes play in promoting the surface change. The contributions ofnatural variability and anthropogenic influences are noted as they combine with the complex nature ofrelationships between the sea ice, the atmosphere, and the ocean to present a challenge to our understandingof the factors underlying recent changes in Antarctic climate. Woven through the discussion isthe realization that establishing and understanding the current changes in Antarctic climate as well asmaking projections of future changes are hampered by the sparsity of observations and the limitationsof climate models. Book Part Antarc* Antarctic Antarctic Peninsula Antarctica Arctic Climate change Sea ice Southern Ocean eCite UTAS (University of Tasmania) Arctic Antarctic Southern Ocean The Antarctic Antarctic Peninsula 241 257
institution Open Polar
collection eCite UTAS (University of Tasmania)
op_collection_id ftunivtasecite
language English
topic Earth Sciences
Climate change science
Climatology
spellingShingle Earth Sciences
Climate change science
Climatology
Raphael, MN
Hobbs, WR
Marshall, GJ
Stammerjohn, SE
Recent climate trends
topic_facet Earth Sciences
Climate change science
Climatology
description In concert with the rest of the world, the climate of Antarctica is changing. This change is seen in keyclimate parameters, such as the atmospheric circulation, surface air temperature, precipitation, sea iceextent, and the temperature of the Southern Ocean. Surface air temperatures are increasing, and indeedfor the second half of the 20th century, the temperature increase on the Antarctic Peninsula was amongthe largest experienced on Earth (Steig et al., 2009). Total sea ice extent is not decreasing, as is occurringin the Arctic, but the deeper levels of the Southern Ocean are warming, similar to most otheroceans. The changes are not uniform in time or space and are due to remote and proximate influences.This chapter discusses the changes in climate at the surface and the deep ocean, including the role thatthe leading atmospheric circulation modes play in promoting the surface change. The contributions ofnatural variability and anthropogenic influences are noted as they combine with the complex nature ofrelationships between the sea ice, the atmosphere, and the ocean to present a challenge to our understandingof the factors underlying recent changes in Antarctic climate. Woven through the discussion isthe realization that establishing and understanding the current changes in Antarctic climate as well asmaking projections of future changes are hampered by the sparsity of observations and the limitationsof climate models.
format Book Part
author Raphael, MN
Hobbs, WR
Marshall, GJ
Stammerjohn, SE
author_facet Raphael, MN
Hobbs, WR
Marshall, GJ
Stammerjohn, SE
author_sort Raphael, MN
title Recent climate trends
title_short Recent climate trends
title_full Recent climate trends
title_fullStr Recent climate trends
title_full_unstemmed Recent climate trends
title_sort recent climate trends
publisher Academic Press
publishDate 2020
url https://www.sciencedirect.com/science/article/pii/B9780128179253000136?via%3Dihub
https://doi.org/10.1016/B978-0-12-817925-3.00013-6
http://ecite.utas.edu.au/145274
geographic Arctic
Antarctic
Southern Ocean
The Antarctic
Antarctic Peninsula
geographic_facet Arctic
Antarctic
Southern Ocean
The Antarctic
Antarctic Peninsula
genre Antarc*
Antarctic
Antarctic Peninsula
Antarctica
Arctic
Climate change
Sea ice
Southern Ocean
genre_facet Antarc*
Antarctic
Antarctic Peninsula
Antarctica
Arctic
Climate change
Sea ice
Southern Ocean
op_relation http://dx.doi.org/10.1016/B978-0-12-817925-3.00013-6
Raphael, MN and Hobbs, WR and Marshall, GJ and Stammerjohn, SE, Recent climate trends, Past Antarctica: Paleoclimatology and Climate Change, Academic Press, M Oliva and J Ruiz-Fernandez (ed), United Kingdom, pp. 241-257. ISBN 9780128179253 (2020) [Research Book Chapter]
9780128179253
http://ecite.utas.edu.au/145274
op_doi https://doi.org/10.1016/B978-0-12-817925-3.00013-6
container_start_page 241
op_container_end_page 257
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