Arctic Stewardship: Maintaining Regional Resilience in an Era of Global Change

That the Arctic is undergoing transformative changes driven in large part by external forces is no longer news. The high latitudes of the Northern Hemisphere, which are not themselves significant sources of anthropogenic emissions of greenhouse gases (GHGs) or short-lived climate pollutants (such as...

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Published in:Ethics & International Affairs
Main Author: Young, Oran R.
Format: Article in Journal/Newspaper
Language:English
Published: Cambridge University Press (CUP) 2012
Subjects:
Ice
Online Access:http://dx.doi.org/10.1017/s0892679412000585
https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0892679412000585
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spelling crcambridgeupr:10.1017/s0892679412000585 2024-03-03T08:36:20+00:00 Arctic Stewardship: Maintaining Regional Resilience in an Era of Global Change Young, Oran R. 2012 http://dx.doi.org/10.1017/s0892679412000585 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0892679412000585 en eng Cambridge University Press (CUP) https://www.cambridge.org/core/terms Ethics & International Affairs volume 26, issue 4, page 407-420 ISSN 0892-6794 1747-7093 Political Science and International Relations Philosophy journal-article 2012 crcambridgeupr https://doi.org/10.1017/s0892679412000585 2024-02-08T08:29:25Z That the Arctic is undergoing transformative changes driven in large part by external forces is no longer news. The high latitudes of the Northern Hemisphere, which are not themselves significant sources of anthropogenic emissions of greenhouse gases (GHGs) or short-lived climate pollutants (such as black carbon soot), are experiencing effects attributable to climate change that are equal to or greater than those occurring in any of the planet's other large regions. Prominent among these effects are rising surface temperatures, a deepening of the active layer of the permafrost, the collapse of sea ice, increases in the intensity of coastal storm surges made possible by the retreat of sea ice, the accelerated melting of the Greenland ice sheet, and the acidification of marine systems. The deposition of black carbon in the high north alone—almost 60 percent of which is thought to originate in Europe—appears to account for half or more of the increase in temperature occurring in the Arctic. Positive feedback processes, such as lowered albedo (that is, the capacity of Earth's surface to reflect incoming solar radiation back into space) following the melting of ice at sea and snow on land, have the effect of magnifying the impact of these external forces. Nowhere is the challenge of adapting to the impacts of climate change more urgent than in Arctic coastal communities confronted with the need to relocate to avoid physical destruction. And nowhere are the threats to individual species (for example, the polar bear) and whole ecosystems more severe than they are in the Arctic, where biophysical changes are outstripping the capacity of plants and animals to adapt to altered conditions. Article in Journal/Newspaper albedo Arctic black carbon Climate change Greenland Ice Ice Sheet permafrost polar bear Sea ice Cambridge University Press Arctic Greenland Ethics & International Affairs 26 4 407 420
institution Open Polar
collection Cambridge University Press
op_collection_id crcambridgeupr
language English
topic Political Science and International Relations
Philosophy
spellingShingle Political Science and International Relations
Philosophy
Young, Oran R.
Arctic Stewardship: Maintaining Regional Resilience in an Era of Global Change
topic_facet Political Science and International Relations
Philosophy
description That the Arctic is undergoing transformative changes driven in large part by external forces is no longer news. The high latitudes of the Northern Hemisphere, which are not themselves significant sources of anthropogenic emissions of greenhouse gases (GHGs) or short-lived climate pollutants (such as black carbon soot), are experiencing effects attributable to climate change that are equal to or greater than those occurring in any of the planet's other large regions. Prominent among these effects are rising surface temperatures, a deepening of the active layer of the permafrost, the collapse of sea ice, increases in the intensity of coastal storm surges made possible by the retreat of sea ice, the accelerated melting of the Greenland ice sheet, and the acidification of marine systems. The deposition of black carbon in the high north alone—almost 60 percent of which is thought to originate in Europe—appears to account for half or more of the increase in temperature occurring in the Arctic. Positive feedback processes, such as lowered albedo (that is, the capacity of Earth's surface to reflect incoming solar radiation back into space) following the melting of ice at sea and snow on land, have the effect of magnifying the impact of these external forces. Nowhere is the challenge of adapting to the impacts of climate change more urgent than in Arctic coastal communities confronted with the need to relocate to avoid physical destruction. And nowhere are the threats to individual species (for example, the polar bear) and whole ecosystems more severe than they are in the Arctic, where biophysical changes are outstripping the capacity of plants and animals to adapt to altered conditions.
format Article in Journal/Newspaper
author Young, Oran R.
author_facet Young, Oran R.
author_sort Young, Oran R.
title Arctic Stewardship: Maintaining Regional Resilience in an Era of Global Change
title_short Arctic Stewardship: Maintaining Regional Resilience in an Era of Global Change
title_full Arctic Stewardship: Maintaining Regional Resilience in an Era of Global Change
title_fullStr Arctic Stewardship: Maintaining Regional Resilience in an Era of Global Change
title_full_unstemmed Arctic Stewardship: Maintaining Regional Resilience in an Era of Global Change
title_sort arctic stewardship: maintaining regional resilience in an era of global change
publisher Cambridge University Press (CUP)
publishDate 2012
url http://dx.doi.org/10.1017/s0892679412000585
https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0892679412000585
geographic Arctic
Greenland
geographic_facet Arctic
Greenland
genre albedo
Arctic
black carbon
Climate change
Greenland
Ice
Ice Sheet
permafrost
polar bear
Sea ice
genre_facet albedo
Arctic
black carbon
Climate change
Greenland
Ice
Ice Sheet
permafrost
polar bear
Sea ice
op_source Ethics & International Affairs
volume 26, issue 4, page 407-420
ISSN 0892-6794 1747-7093
op_rights https://www.cambridge.org/core/terms
op_doi https://doi.org/10.1017/s0892679412000585
container_title Ethics & International Affairs
container_volume 26
container_issue 4
container_start_page 407
op_container_end_page 420
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