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Global eight drought types: Spatio-temporal characteristics and vegetation response.
Ji, Yongyue; Zeng, Sidong; Yang, Linhan; Wan, Hui; Xia, Jun.
  • Ji Y; Chongqing Institute of Green and Intelligent Technology, Chinese Academy of Sciences, Chongqing, 400714, China; Chongqing School, University of Chinese Academy of Sciences, Chongqing, 400714, China; Changjiang Institute of Survey, Planning, Design and Research Corporation, Key Laboratory of Water Gr
  • Zeng S; Chongqing Institute of Green and Intelligent Technology, Chinese Academy of Sciences, Chongqing, 400714, China; Chongqing School, University of Chinese Academy of Sciences, Chongqing, 400714, China. Electronic address: zengsidong@cigit.ac.cn.
  • Yang L; Chongqing Institute of Green and Intelligent Technology, Chinese Academy of Sciences, Chongqing, 400714, China; Chongqing School, University of Chinese Academy of Sciences, Chongqing, 400714, China; Changjiang Institute of Survey, Planning, Design and Research Corporation, Key Laboratory of Water Gr
  • Wan H; Changjiang Institute of Survey, Planning, Design and Research Corporation, Key Laboratory of Water Grid Project and Regulation of Ministry of Water Resources, Wuhan, 430010, China.
  • Xia J; State Key Laboratory of Water Resources Engineering and Management, Wuhan University, Wuhan, 430072, China.
J Environ Manage ; 359: 121069, 2024 May.
Article en En | MEDLINE | ID: mdl-38714034
ABSTRACT
The traditional classification of drought events into seasonal and flash types oversimplified the complexity and variability of global drought phenomena, limiting a deeper understanding of drought characteristics and their impacts on vegetation. To address this issue, soil moisture percentile methods and the Soil Moisture Anomaly Percentage Index (SMAPI) were employed to create time series for flash drought (FD) and seasonal drought (SD) events globally from 1981 to 2020. A novel categorization framework was proposed to subdivide the two basic drought categories into eight distinct drought types using a set relationship identification method. The results showed fluctuating trends in the frequencies of Independent FD and Inclusion FD, which declined rapidly after 2011 at rates of 0.05 and 0.04 times/year, respectively. Independent FD frequency was highest in humid areas and decreased with increasing aridity. The spatial distributions of Inclusion FD and SD were similar, with both frequencies highest in extremely arid areas and decreasing with increasing humidity. The frequency of Independent SD, which peaked in semi-arid areas, increased significantly after 2011 at a rate of 0.01 times/year. The occurrence of FD evolving into SD or emerging at the end of SD was rare, with a global average of 0.46 events/decade and little spatial variation. Between 1981 and 2020, FD showed a U-shaped trend in drought duration, while SD showed no clear pattern. The duration of FD showed little difference across arid and humid zones, but the duration of SD decreased significantly with increasing humidity. Vegetation responses to drought varied, with arid regions showing longer response time compared to humid regions. A positive correlation between temperature and solar-induced chlorophyll fluorescence (SIF) during droughts was observed, while precipitation generally showed a negative correlation with SIF. Radiation had a minimal effect on SIF during droughts. The study offered a comprehensive categorization of drought events, enhancing our understanding of their spatiotemporal characteristics and vegetation responses on a global scale.
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Texto completo: 1 Banco de datos: MEDLINE Asunto principal: Sequías Idioma: En Año: 2024 Tipo del documento: Article

Texto completo: 1 Banco de datos: MEDLINE Asunto principal: Sequías Idioma: En Año: 2024 Tipo del documento: Article