Global S&T Development Trend Analysis Platform of Resources and Environment
DOI | 10.1007/s00382-016-3101-z |
Moisture increase in response to high-altitude warming evidenced by tree-rings on the southeastern Tibetan Plateau | |
Li, Jinbao1; Shi, Jiangfeng2; Zhang, David D.1; Yang, Bao3; Fang, Keyan4; Yue, Pak Hong1 | |
2017 | |
发表期刊 | CLIMATE DYNAMICS
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ISSN | 0930-7575 |
EISSN | 1432-0894 |
出版年 | 2017 |
卷号 | 48 |
文章类型 | Article |
语种 | 英语 |
国家 | Peoples R China |
英文摘要 | Rapid warming has been observed in the high-altitude areas around the globe, but the implications on moisture change are not fully understood. Here we use tree-rings to reveal common moisture change on the southeastern Tibetan Plateau (TP) during the past five centuries, and show that regional moisture change in late spring to early summer (April-June) is closely related to large-scale temperature anomaly over the TP, with increased moisture coincident with periods of high temperature. The most recent pluvial during the 1990s-2000s is likely the wettest for the past five centuries, which coincides with the warmest period on the TP during the past millennium. Dynamic analysis reveals that vertical air convection is enhanced in response to anomalous TP surface warming, leading to an increase in lower-tropospheric humidity and effective precipitation over the southeastern TP. The coherent warm-wet relationship identified in both tree-rings and dynamic analysis implies a generally wetter condition on the southeastern TP under future warming. |
英文关键词 | Dendrochronology High-altitude warming Moisture change Tibetan Plateau |
领域 | 气候变化 |
收录类别 | SCI-E |
WOS记录号 | WOS:000392307300037 |
WOS关键词 | ASIAN SUMMER MONSOON ; CENTRAL HENGDUAN MOUNTAINS ; DELAYED SPRING PHENOLOGY ; DROUGHT RECONSTRUCTION ; CLIMATE-CHANGE ; ERA-INTERIM ; CHINA ; TEMPERATURE ; PRECIPITATION ; REGIONS |
WOS类目 | Meteorology & Atmospheric Sciences |
WOS研究方向 | Meteorology & Atmospheric Sciences |
引用统计 | |
文献类型 | 期刊论文 |
条目标识符 | http://119.78.100.173/C666/handle/2XK7JSWQ/36310 |
专题 | 气候变化 |
作者单位 | 1.Univ Hong Kong, Dept Geog, Pokfulam, Hong Kong, Peoples R China; 2.Nanjing Univ, Inst Climate & Global Change Res, Sch Geog & Oceanog Sci, Nanjing 210023, Jiangsu, Peoples R China; 3.Chinese Acad Sci, Cold & Arid Reg Environm & Engn Res Inst, Key Lab Desert & Desertificat, Lanzhou 730000, Peoples R China; 4.Fujian Normal Univ, Coll Geog Sci, Key Lab Humid Subtrop Ecogeog Proc, Minist Educ, Fuzhou 350007, Peoples R China |
推荐引用方式 GB/T 7714 | Li, Jinbao,Shi, Jiangfeng,Zhang, David D.,et al. Moisture increase in response to high-altitude warming evidenced by tree-rings on the southeastern Tibetan Plateau[J]. CLIMATE DYNAMICS,2017,48. |
APA | Li, Jinbao,Shi, Jiangfeng,Zhang, David D.,Yang, Bao,Fang, Keyan,&Yue, Pak Hong.(2017).Moisture increase in response to high-altitude warming evidenced by tree-rings on the southeastern Tibetan Plateau.CLIMATE DYNAMICS,48. |
MLA | Li, Jinbao,et al."Moisture increase in response to high-altitude warming evidenced by tree-rings on the southeastern Tibetan Plateau".CLIMATE DYNAMICS 48(2017). |
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