The urgency of Arctic change

This article provides a synthesis of the latest observational trends and projections for the future of the Arctic. First, the Arctic is already changing rapidly as a result of climate change. Contemporary warm Arctic temperatures and large sea ice deficits (75% volume loss) demonstrate climate state...

Full description

Bibliographic Details
Published in:Polar Science
Format: Article in Journal/Newspaper
Language:English
Published: 2019
Subjects:
Ice
Online Access:https://nipr.repo.nii.ac.jp/?action=repository_uri&item_id=15911
http://id.nii.ac.jp/1291/00015805/
id ftnipr:oai:nipr.repo.nii.ac.jp:00015911
record_format openpolar
spelling ftnipr:oai:nipr.repo.nii.ac.jp:00015911 2023-05-15T14:30:58+02:00 The urgency of Arctic change 2019-09 https://nipr.repo.nii.ac.jp/?action=repository_uri&item_id=15911 http://id.nii.ac.jp/1291/00015805/ en eng https://doi.org/10.1016/j.polar.2018.11.008 https://nipr.repo.nii.ac.jp/?action=repository_uri&item_id=15911 http://id.nii.ac.jp/1291/00015805/ Polar Science, 21, 6-13(2019-09) 18739652 Arctic Global change Sea ice Climate projections 2 °C limit Cryosphere Journal Article 2019 ftnipr https://doi.org/10.1016/j.polar.2018.11.008 2022-12-03T19:43:10Z This article provides a synthesis of the latest observational trends and projections for the future of the Arctic. First, the Arctic is already changing rapidly as a result of climate change. Contemporary warm Arctic temperatures and large sea ice deficits (75% volume loss) demonstrate climate states outside of previous experience. Modeled changes of the Arctic cryosphere demonstrate that even limiting global temperature increases to near 2 °C will leave the Arctic a much different environment by mid-century with less snow and sea ice, melted permafrost, altered ecosystems, and a projected annual mean Arctic temperature increase of +4 °C. Second, even under ambitious emission reduction scenarios, high-latitude land ice melt, including Greenland, are foreseen to continue due to internal lags, leading to accelerating global sea level rise throughout the century. Third, future Arctic changes may in turn impact lower latitudes through tundra greenhouse gas release and shifts in ocean and atmospheric circulation. Arctic-specific radiative and heat storage feedbacks may become an obstacle to achieving a stabilized global climate. In light of these trends, the precautionary principle calls for early adaptation and mitigation actions. Article in Journal/Newspaper arctic cryosphere Arctic Climate change Greenland Ice permafrost Polar Science Polar Science Sea ice Tundra National Institute of Polar Research Repository, Japan Arctic Greenland Polar Science 21 6 13
institution Open Polar
collection National Institute of Polar Research Repository, Japan
op_collection_id ftnipr
language English
topic Arctic
Global change
Sea ice
Climate projections
2 °C limit
Cryosphere
spellingShingle Arctic
Global change
Sea ice
Climate projections
2 °C limit
Cryosphere
The urgency of Arctic change
topic_facet Arctic
Global change
Sea ice
Climate projections
2 °C limit
Cryosphere
description This article provides a synthesis of the latest observational trends and projections for the future of the Arctic. First, the Arctic is already changing rapidly as a result of climate change. Contemporary warm Arctic temperatures and large sea ice deficits (75% volume loss) demonstrate climate states outside of previous experience. Modeled changes of the Arctic cryosphere demonstrate that even limiting global temperature increases to near 2 °C will leave the Arctic a much different environment by mid-century with less snow and sea ice, melted permafrost, altered ecosystems, and a projected annual mean Arctic temperature increase of +4 °C. Second, even under ambitious emission reduction scenarios, high-latitude land ice melt, including Greenland, are foreseen to continue due to internal lags, leading to accelerating global sea level rise throughout the century. Third, future Arctic changes may in turn impact lower latitudes through tundra greenhouse gas release and shifts in ocean and atmospheric circulation. Arctic-specific radiative and heat storage feedbacks may become an obstacle to achieving a stabilized global climate. In light of these trends, the precautionary principle calls for early adaptation and mitigation actions.
format Article in Journal/Newspaper
title The urgency of Arctic change
title_short The urgency of Arctic change
title_full The urgency of Arctic change
title_fullStr The urgency of Arctic change
title_full_unstemmed The urgency of Arctic change
title_sort urgency of arctic change
publishDate 2019
url https://nipr.repo.nii.ac.jp/?action=repository_uri&item_id=15911
http://id.nii.ac.jp/1291/00015805/
geographic Arctic
Greenland
geographic_facet Arctic
Greenland
genre arctic cryosphere
Arctic
Climate change
Greenland
Ice
permafrost
Polar Science
Polar Science
Sea ice
Tundra
genre_facet arctic cryosphere
Arctic
Climate change
Greenland
Ice
permafrost
Polar Science
Polar Science
Sea ice
Tundra
op_relation https://doi.org/10.1016/j.polar.2018.11.008
https://nipr.repo.nii.ac.jp/?action=repository_uri&item_id=15911
http://id.nii.ac.jp/1291/00015805/
Polar Science, 21, 6-13(2019-09)
18739652
op_doi https://doi.org/10.1016/j.polar.2018.11.008
container_title Polar Science
container_volume 21
container_start_page 6
op_container_end_page 13
_version_ 1766304720134078464