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...
| 出版年: | Environmental Research Letters |
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| 主要な著者: | , , , |
| フォーマット: | 論文 |
| 言語: | 英語 |
| 出版事項: |
IOP Publishing
2020-01-01
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| 主題: | |
| オンライン・アクセス: | https://doi.org/10.1088/1748-9326/ab5e01 |
| _version_ | 1850296863738036224 |
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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. |
| format | Article |
| id | doaj-art-c67bb8acd29849e596b9319be4f1c4e9 |
| institution | Directory of Open Access Journals |
| issn | 1748-9326 |
| language | English |
| publishDate | 2020-01-01 |
| publisher | IOP Publishing |
| record_format | Article |
| 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 |
| work_keys_str_mv | AT jianpingduan unprecedentedrecentlatesummerwarmextremesrecordedintreeringdensityonthetibetanplateau AT peiliwu unprecedentedrecentlatesummerwarmextremesrecordedintreeringdensityonthetibetanplateau AT zhuguoma unprecedentedrecentlatesummerwarmextremesrecordedintreeringdensityonthetibetanplateau AT yawenduan unprecedentedrecentlatesummerwarmextremesrecordedintreeringdensityonthetibetanplateau |
