Unprecedented recent late-summer warm extremes recorded in tree-ring density on the Tibetan Plateau

Tree-ring records have shown a significant upward trend of late summer temperatures over the Tibetan Plateau (TP) in recent decades. More detailed instrumental observations over the TP have also shown an increase in warm extremes, especially in the high-altitude area. It is not clear whether the rec...

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出版年:Environmental Research Letters
主要な著者: Jianping Duan, Peili Wu, Zhuguo Ma, Yawen Duan
フォーマット: 論文
言語:英語
出版事項: IOP Publishing 2020-01-01
主題:
オンライン・アクセス:https://doi.org/10.1088/1748-9326/ab5e01
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author Jianping Duan
Peili Wu
Zhuguo Ma
Yawen Duan
author_facet Jianping Duan
Peili Wu
Zhuguo Ma
Yawen Duan
author_sort Jianping Duan
collection DOAJ
container_title Environmental Research Letters
description Tree-ring records have shown a significant upward trend of late summer temperatures over the Tibetan Plateau (TP) in recent decades. More detailed instrumental observations over the TP have also shown an increase in warm extremes, especially in the high-altitude area. It is not clear whether the recent increase in occurrence of warm extremes on the TP reflects an amplification of recent temperature fluctuations or it relates to the long-term climate trend. This study aims to address the above question by analyzing long-term late summer (August–September) temperature extremes over the TP using temperature reconstructions derived from tree-ring maximum latewood density. Our results show that the recent frequency of late summer warm extremes was unprecedented over the past four centuries, while the occurrence of cold extremes in the instrumental interval was minimal. However, after the removal of long-term trend, the frequencies of both warm and cold extremes in the instrumental period are actually smaller than the pre-instrumental period, indicating a decreased variability of late summer temperatures. Thus, we conclude that the recent observed increase in warm extremes is related to the long-term warming trend, rather than an amplification of temperature variability. This finding implies that the persistent warming on the TP in the future might trigger much more frequent warm extremes with potential ecological and environmental effects.
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spelling doaj-art-c67bb8acd29849e596b9319be4f1c4e92025-08-19T23:32:49ZengIOP PublishingEnvironmental Research Letters1748-93262020-01-0115202400610.1088/1748-9326/ab5e01Unprecedented recent late-summer warm extremes recorded in tree-ring density on the Tibetan PlateauJianping Duan0https://orcid.org/0000-0002-0095-0714Peili Wu1https://orcid.org/0000-0001-7908-7062Zhuguo Ma2https://orcid.org/0000-0002-3968-7837Yawen Duan3https://orcid.org/0000-0002-9011-5412CAS Key Laboratory of Regional Climate-Environment for Temperate East Asia, Institute of Atmospheric Physics, Chinese Academy of Sciences, 100029 Beijing, People’s Republic of ChinaMet Office Hadley Centre, Exeter EX1 3PB, United KingdomCAS Key Laboratory of Regional Climate-Environment for Temperate East Asia, Institute of Atmospheric Physics, Chinese Academy of Sciences, 100029 Beijing, People’s Republic of China; University of Chinese Academy of Sciences , 100049 Beijing, People’s Republic of ChinaCAS Key Laboratory of Regional Climate-Environment for Temperate East Asia, Institute of Atmospheric Physics, Chinese Academy of Sciences, 100029 Beijing, People’s Republic of ChinaTree-ring records have shown a significant upward trend of late summer temperatures over the Tibetan Plateau (TP) in recent decades. More detailed instrumental observations over the TP have also shown an increase in warm extremes, especially in the high-altitude area. It is not clear whether the recent increase in occurrence of warm extremes on the TP reflects an amplification of recent temperature fluctuations or it relates to the long-term climate trend. This study aims to address the above question by analyzing long-term late summer (August–September) temperature extremes over the TP using temperature reconstructions derived from tree-ring maximum latewood density. Our results show that the recent frequency of late summer warm extremes was unprecedented over the past four centuries, while the occurrence of cold extremes in the instrumental interval was minimal. However, after the removal of long-term trend, the frequencies of both warm and cold extremes in the instrumental period are actually smaller than the pre-instrumental period, indicating a decreased variability of late summer temperatures. Thus, we conclude that the recent observed increase in warm extremes is related to the long-term warming trend, rather than an amplification of temperature variability. This finding implies that the persistent warming on the TP in the future might trigger much more frequent warm extremes with potential ecological and environmental effects.https://doi.org/10.1088/1748-9326/ab5e01temperature extremestree-ring densityTibetan Plateauclimate changetemperature variability
spellingShingle Jianping Duan
Peili Wu
Zhuguo Ma
Yawen Duan
Unprecedented recent late-summer warm extremes recorded in tree-ring density on the Tibetan Plateau
temperature extremes
tree-ring density
Tibetan Plateau
climate change
temperature variability
title Unprecedented recent late-summer warm extremes recorded in tree-ring density on the Tibetan Plateau
title_full Unprecedented recent late-summer warm extremes recorded in tree-ring density on the Tibetan Plateau
title_fullStr Unprecedented recent late-summer warm extremes recorded in tree-ring density on the Tibetan Plateau
title_full_unstemmed Unprecedented recent late-summer warm extremes recorded in tree-ring density on the Tibetan Plateau
title_short Unprecedented recent late-summer warm extremes recorded in tree-ring density on the Tibetan Plateau
title_sort unprecedented recent late summer warm extremes recorded in tree ring density on the tibetan plateau
topic temperature extremes
tree-ring density
Tibetan Plateau
climate change
temperature variability
url https://doi.org/10.1088/1748-9326/ab5e01
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