The twenty-first century Arctic environment: accelerating change in the atmospheric, oceanic and terrestrial spheres

The Arctic possesses distinctive environmental characteristics that act as strong, positive feedbacks on atmospheric warming; in fact, it is almost uniquely susceptible to rapid change brought about through climate warming from both natural and anthropogenic sources. The aim of this commentary is to...

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Main Author: Richard Hodgkins
Format: Other Non-Article Part of Journal/Newspaper
Language:unknown
Published: 2014
Subjects:
Ice
Online Access:https://figshare.com/articles/journal_contribution/The_twenty-first_century_Arctic_environment_accelerating_change_in_the_atmospheric_oceanic_and_terrestrial_spheres/9483245
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spelling ftloughboroughun:oai:figshare.com:article/9483245 2023-05-15T14:33:22+02:00 The twenty-first century Arctic environment: accelerating change in the atmospheric, oceanic and terrestrial spheres Richard Hodgkins 2014-01-01T00:00:00Z https://figshare.com/articles/journal_contribution/The_twenty-first_century_Arctic_environment_accelerating_change_in_the_atmospheric_oceanic_and_terrestrial_spheres/9483245 unknown 2134/24105 https://figshare.com/articles/journal_contribution/The_twenty-first_century_Arctic_environment_accelerating_change_in_the_atmospheric_oceanic_and_terrestrial_spheres/9483245 CC BY-NC-ND 4.0 CC-BY-NC-ND Earth Sciences not elsewhere classified Arctic Climate change Arctic amplification Sea ice Permafrost Cryosphere Text Journal contribution 2014 ftloughboroughun 2022-01-01T20:12:06Z The Arctic possesses distinctive environmental characteristics that act as strong, positive feedbacks on atmospheric warming; in fact, it is almost uniquely susceptible to rapid change brought about through climate warming from both natural and anthropogenic sources. The aim of this commentary is to outline recent and probable future environmental changes in the Arctic. It commences with a consideration of rates of change through the satellite era in air temperatures, sea ice extent, snow cover and the state of balance of the Greenland Ice Sheet. This is subsequently set against fluctuations over previous centuries and millennia. From this observational basis, the commentary moves on to consider factors which particularly amplify rates of change in high northern latitudes, before addressing further feedbacks which may become important, and how Arctic changes may proceed up to the year 2100. Other Non-Article Part of Journal/Newspaper Arctic Climate change Greenland Ice Ice Sheet permafrost Sea ice Loughborough University: Figshare Arctic Greenland
institution Open Polar
collection Loughborough University: Figshare
op_collection_id ftloughboroughun
language unknown
topic Earth Sciences not elsewhere classified
Arctic
Climate change
Arctic amplification
Sea ice
Permafrost
Cryosphere
spellingShingle Earth Sciences not elsewhere classified
Arctic
Climate change
Arctic amplification
Sea ice
Permafrost
Cryosphere
Richard Hodgkins
The twenty-first century Arctic environment: accelerating change in the atmospheric, oceanic and terrestrial spheres
topic_facet Earth Sciences not elsewhere classified
Arctic
Climate change
Arctic amplification
Sea ice
Permafrost
Cryosphere
description The Arctic possesses distinctive environmental characteristics that act as strong, positive feedbacks on atmospheric warming; in fact, it is almost uniquely susceptible to rapid change brought about through climate warming from both natural and anthropogenic sources. The aim of this commentary is to outline recent and probable future environmental changes in the Arctic. It commences with a consideration of rates of change through the satellite era in air temperatures, sea ice extent, snow cover and the state of balance of the Greenland Ice Sheet. This is subsequently set against fluctuations over previous centuries and millennia. From this observational basis, the commentary moves on to consider factors which particularly amplify rates of change in high northern latitudes, before addressing further feedbacks which may become important, and how Arctic changes may proceed up to the year 2100.
format Other Non-Article Part of Journal/Newspaper
author Richard Hodgkins
author_facet Richard Hodgkins
author_sort Richard Hodgkins
title The twenty-first century Arctic environment: accelerating change in the atmospheric, oceanic and terrestrial spheres
title_short The twenty-first century Arctic environment: accelerating change in the atmospheric, oceanic and terrestrial spheres
title_full The twenty-first century Arctic environment: accelerating change in the atmospheric, oceanic and terrestrial spheres
title_fullStr The twenty-first century Arctic environment: accelerating change in the atmospheric, oceanic and terrestrial spheres
title_full_unstemmed The twenty-first century Arctic environment: accelerating change in the atmospheric, oceanic and terrestrial spheres
title_sort twenty-first century arctic environment: accelerating change in the atmospheric, oceanic and terrestrial spheres
publishDate 2014
url https://figshare.com/articles/journal_contribution/The_twenty-first_century_Arctic_environment_accelerating_change_in_the_atmospheric_oceanic_and_terrestrial_spheres/9483245
geographic Arctic
Greenland
geographic_facet Arctic
Greenland
genre Arctic
Climate change
Greenland
Ice
Ice Sheet
permafrost
Sea ice
genre_facet Arctic
Climate change
Greenland
Ice
Ice Sheet
permafrost
Sea ice
op_relation 2134/24105
https://figshare.com/articles/journal_contribution/The_twenty-first_century_Arctic_environment_accelerating_change_in_the_atmospheric_oceanic_and_terrestrial_spheres/9483245
op_rights CC BY-NC-ND 4.0
op_rightsnorm CC-BY-NC-ND
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