中国科学院机构知识库网格
Chinese Academy of Sciences Institutional Repositories Grid
Interannual moisture variability on the Qinghai Plateau: Trends, patterns, and implications

文献类型:期刊论文

作者Yang, Yanxi3; Wang, Junbang3; Zhang, Xiujuan2; Ye, Hui1; Yuan, Bin1; Watson, Alan E.3
刊名JOURNAL OF HYDROLOGY
出版日期2024-12-01
卷号645页码:132074
关键词Climate change Moisture Index (IM) Quasi-periodic EEMD Qinghai Plateau (QP)
DOI10.1016/j.jhydrol.2024.132074
产权排序1
文献子类Article
英文摘要Investigating surface dry-wet patterns on the Qinghai Plateau (QP) is crucial for water allocation, ecological sustainability, and climate variability adaptation strategies. Existing discrepancies in the QP dry-wet trends and distribution characteristics underscored the need for a more refined analysis. This study utilized the Thornthwaite Moisture Index (IM) to quantify changes in surface dryness and wetness under prevailing climatic conditions. Linear trend regression and ensemble empirical mode decomposition (EEMD) were applied to study the dynamic and periodic characteristics of the QP from 1980 to 2018. Our findings revealed a decrease from southeast to northwest in IM, with the semi-arid and sub-humid transition line aligning closely with the 400 mm isohyet. The dry-wet transition line exhibited a northwestward trend over the past four decades. Possibly influenced by monsoon circulation and El Nino-Southern Oscillation (ENSO), the annual IM displayed a quasi-cycle of 3 to 5 years, manifested by a dry period (1990-2004) and a wet period (2005-2012). However, spatial differences existed, challenging the universality of the Dry gets Drier and Wet gets Wetter (DDWW) pattern. Precipitation (PRCP) changes could predict over 90 % of IM spatiotemporal variations. Additionally, the IM response to Average Temperature (TAVG) exhibited an inverted U-shaped curve, with a boundary (-3.8 degrees C) below which cooler regions became wetter and above which they became drier. The observed warming and precipitation shifts suggested that continued warming could lead to warmer and wetter climates, potentially causing ecological and environmental problems. Therefore, examining the surface moisture budget is of critical scientific and practical significance, in order to provide a decision- making basis for mitigating and adapting to climate change.
WOS关键词TIBETAN PLATEAU ; DROUGHT ; CHINA ; EVAPOTRANSPIRATION ; HYDROCLIMATE ; ROBUST
WOS研究方向Engineering ; Geology ; Water Resources
WOS记录号WOS:001345747400001
源URL[http://ir.igsnrr.ac.cn/handle/311030/209542]  
专题生态系统网络观测与模拟院重点实验室_外文论文
通讯作者Wang, Junbang
作者单位1.Jiujiang Univ, Sch Tourism & Geog, Jiujiang 332005, Peoples R China
2.Yangtze Univ, Coll Hort & Landscape Architecture, Jingzhou 434025, Peoples R China
3.[Yang, Yanxi; Wang, Junbang; Watson, Alan E.] Chinese Acad Sci, Inst Geog Sci & Nat Resources Res, Natl Ecosyst Sci Data Ctr, Key Lab Ecosyst Network Observat & Modeling, 11A Datun Rd, Beijing 100101, Peoples R China
推荐引用方式
GB/T 7714
Yang, Yanxi,Wang, Junbang,Zhang, Xiujuan,et al. Interannual moisture variability on the Qinghai Plateau: Trends, patterns, and implications[J]. JOURNAL OF HYDROLOGY,2024,645:132074.
APA Yang, Yanxi,Wang, Junbang,Zhang, Xiujuan,Ye, Hui,Yuan, Bin,&Watson, Alan E..(2024).Interannual moisture variability on the Qinghai Plateau: Trends, patterns, and implications.JOURNAL OF HYDROLOGY,645,132074.
MLA Yang, Yanxi,et al."Interannual moisture variability on the Qinghai Plateau: Trends, patterns, and implications".JOURNAL OF HYDROLOGY 645(2024):132074.

入库方式: OAI收割

来源:地理科学与资源研究所

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