Reduced Risks of Temperature Extremes From 0.5°C less Global Warming in the Earth's Three Poles

Abstract Future projection of temperature extremes in the “Earth's three poles” (the Arctic, Antarctica, and Third Pole‐Tibetan Plateau [TP]) is of importance to risk assessment and policymaking owing to the high sensitivity to climate change in these regions. In this study, future projections...

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Published in:Earth's Future
Main Authors: Bin Tang, Wenting Hu, Anmin Duan, Kailun Gao, Yuzuo Peng
Format: Article in Journal/Newspaper
Language:English
Published: Wiley 2022
Subjects:
geo
Online Access:https://doi.org/10.1029/2021EF002525
https://doaj.org/article/fc0bee269fa24a7ba6f093de0c455784
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spelling fttriple:oai:gotriple.eu:oai:doaj.org/article:fc0bee269fa24a7ba6f093de0c455784 2023-05-15T13:39:34+02:00 Reduced Risks of Temperature Extremes From 0.5°C less Global Warming in the Earth's Three Poles Bin Tang Wenting Hu Anmin Duan Kailun Gao Yuzuo Peng 2022-02-01 https://doi.org/10.1029/2021EF002525 https://doaj.org/article/fc0bee269fa24a7ba6f093de0c455784 en eng Wiley 2328-4277 doi:10.1029/2021EF002525 https://doaj.org/article/fc0bee269fa24a7ba6f093de0c455784 undefined Earth's Future, Vol 10, Iss 2, Pp n/a-n/a (2022) geo archi Journal Article https://vocabularies.coar-repositories.org/resource_types/c_6501/ 2022 fttriple https://doi.org/10.1029/2021EF002525 2023-01-22T18:19:36Z Abstract Future projection of temperature extremes in the “Earth's three poles” (the Arctic, Antarctica, and Third Pole‐Tibetan Plateau [TP]) is of importance to risk assessment and policymaking owing to the high sensitivity to climate change in these regions. In this study, future projections of four extreme temperature indices were constructed after the application of a bias correction method in models of Phase 6 of the Coupled Model Intercomparison Project (CMIP6). The reduced intensification of temperature extremes in the Earth's three poles if warming can be limited to 1.5°C instead of 2°C above the pre‐industrial level was examined. Results showed that all the extreme temperature indices show significant increasing trends under both the SSP2–4.5 and SSP5–8.5 scenarios over the Earth's three poles (SSP: Shared Socioeconomic Pathway). For the coldest night (TNn), warmest night (TNx), and warmest day (TXx), the greatest increase by the end of the 21st century under SSP5–8.5 occurs in the Arctic, followed by the TP and finally Antarctica. For the coldest day (TXn), the greatest increase occurs in the Arctic, followed by Antarctica and finally the TP. If global warming can be limited to 1.5°C rather than 2°C, the intensification of TNn, TNx, TXn, and TXx in the Arctic (Antarctica/TP) under SSP5–8.5 is projected to reduce by 66% (21.7%/44.26%), 50.31% (54.79%/60.52%), 71.58% (12.91%/65.81%), and 41.73% (81.3%/57.34%), respectively, and the results are similar for SSP2–4.5. Therefore, keeping a lower warming target is essential for reducing the risk of extreme events in the Earth's three poles. Article in Journal/Newspaper Antarc* Antarctica Arctic Climate change Global warming Unknown Arctic Earth's Future 10 2
institution Open Polar
collection Unknown
op_collection_id fttriple
language English
topic geo
archi
spellingShingle geo
archi
Bin Tang
Wenting Hu
Anmin Duan
Kailun Gao
Yuzuo Peng
Reduced Risks of Temperature Extremes From 0.5°C less Global Warming in the Earth's Three Poles
topic_facet geo
archi
description Abstract Future projection of temperature extremes in the “Earth's three poles” (the Arctic, Antarctica, and Third Pole‐Tibetan Plateau [TP]) is of importance to risk assessment and policymaking owing to the high sensitivity to climate change in these regions. In this study, future projections of four extreme temperature indices were constructed after the application of a bias correction method in models of Phase 6 of the Coupled Model Intercomparison Project (CMIP6). The reduced intensification of temperature extremes in the Earth's three poles if warming can be limited to 1.5°C instead of 2°C above the pre‐industrial level was examined. Results showed that all the extreme temperature indices show significant increasing trends under both the SSP2–4.5 and SSP5–8.5 scenarios over the Earth's three poles (SSP: Shared Socioeconomic Pathway). For the coldest night (TNn), warmest night (TNx), and warmest day (TXx), the greatest increase by the end of the 21st century under SSP5–8.5 occurs in the Arctic, followed by the TP and finally Antarctica. For the coldest day (TXn), the greatest increase occurs in the Arctic, followed by Antarctica and finally the TP. If global warming can be limited to 1.5°C rather than 2°C, the intensification of TNn, TNx, TXn, and TXx in the Arctic (Antarctica/TP) under SSP5–8.5 is projected to reduce by 66% (21.7%/44.26%), 50.31% (54.79%/60.52%), 71.58% (12.91%/65.81%), and 41.73% (81.3%/57.34%), respectively, and the results are similar for SSP2–4.5. Therefore, keeping a lower warming target is essential for reducing the risk of extreme events in the Earth's three poles.
format Article in Journal/Newspaper
author Bin Tang
Wenting Hu
Anmin Duan
Kailun Gao
Yuzuo Peng
author_facet Bin Tang
Wenting Hu
Anmin Duan
Kailun Gao
Yuzuo Peng
author_sort Bin Tang
title Reduced Risks of Temperature Extremes From 0.5°C less Global Warming in the Earth's Three Poles
title_short Reduced Risks of Temperature Extremes From 0.5°C less Global Warming in the Earth's Three Poles
title_full Reduced Risks of Temperature Extremes From 0.5°C less Global Warming in the Earth's Three Poles
title_fullStr Reduced Risks of Temperature Extremes From 0.5°C less Global Warming in the Earth's Three Poles
title_full_unstemmed Reduced Risks of Temperature Extremes From 0.5°C less Global Warming in the Earth's Three Poles
title_sort reduced risks of temperature extremes from 0.5°c less global warming in the earth's three poles
publisher Wiley
publishDate 2022
url https://doi.org/10.1029/2021EF002525
https://doaj.org/article/fc0bee269fa24a7ba6f093de0c455784
geographic Arctic
geographic_facet Arctic
genre Antarc*
Antarctica
Arctic
Climate change
Global warming
genre_facet Antarc*
Antarctica
Arctic
Climate change
Global warming
op_source Earth's Future, Vol 10, Iss 2, Pp n/a-n/a (2022)
op_relation 2328-4277
doi:10.1029/2021EF002525
https://doaj.org/article/fc0bee269fa24a7ba6f093de0c455784
op_rights undefined
op_doi https://doi.org/10.1029/2021EF002525
container_title Earth's Future
container_volume 10
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