Global S&T Development Trend Analysis Platform of Resources and Environment
DOI | 10.1002/2016GL071768 |
Spatiotemporal dynamics of global drought | |
Herrera-Estrada, Julio E.1; Satoh, Yusuke2; Sheffield, Justin1,3 | |
2017-03-16 | |
发表期刊 | GEOPHYSICAL RESEARCH LETTERS
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ISSN | 0094-8276 |
EISSN | 1944-8007 |
出版年 | 2017 |
卷号 | 44期号:5 |
文章类型 | Article |
语种 | 英语 |
国家 | USA; Austria; England |
英文摘要 | Understanding the evolution and physical drivers of drought is critical to informing forecasting efforts. One aspect that has seldom been explored is the joint evolution of droughts in space and time. Most studies fix the reference area and focus on their temporal variability or study their spatial heterogeneity over fixed durations. This work implements a Lagrangian approach by aggregating contiguous areas under drought into clusters. These clusters become the frame of reference and are tracked as they evolve through space and time. Clusters were identified from soil moisture data from the Climate Forecast System Reanalysis (1979-2009). Evapotranspiration, moisture fluxes, and precipitation were used to explore the relevance of possible mechanisms of drought propagation. While most droughts remain near their origin, the centroid of 10% of clusters traveled at least 1400-3100km, depending on the continent. This approach also revealed that large-scale droughts often lock into further growth and intensification. Plain Language Summary Droughts are some of the most expensive natural disasters that society has to face, so understanding how they evolve and what are the physical mechanisms that control them is critical for improving our ability to predict them. Past research has focused mostly on how droughts evolve in time over a fixed region and how droughts of a given duration evolve in space. However, little work has been done to study how they evolve in time and space, simultaneously, leading to a significant gap in our understanding of these extreme events. In this work we identify individual drought events between 1979 and 2009 around the world and track them in space and time to analyze their characteristics and behaviors across different continents. We find that some droughts can travel hundreds of kilometers from where they originated (e.g., from the U.S. Southwest to the U.S. Midwest), and that after droughts have grown and become intense enough, they will tend to become even larger and more intense before conditions improve (i.e., conditions will tend to become worse before they become better). |
领域 | 气候变化 |
收录类别 | SCI-E |
WOS记录号 | WOS:000398183700024 |
WOS关键词 | UNITED-STATES ; SOIL-MOISTURE ; TEMPORAL VARIABILITY ; NONLINEAR DYNAMICS ; CLIMATE SCALES ; SUMMER DROUGHT ; TIME SCALES ; PATTERNS ; 20TH-CENTURY ; REANALYSIS |
WOS类目 | Geosciences, Multidisciplinary |
WOS研究方向 | Geology |
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/25806 |
专题 | 气候变化 |
作者单位 | 1.Princeton Univ, Dept Civil & Environm Engn, Princeton, NJ 08544 USA; 2.Int Inst Appl Syst Anal, Laxenburg, Austria; 3.Univ Southampton, Geog & Environm, Southampton, Hants, England |
推荐引用方式 GB/T 7714 | Herrera-Estrada, Julio E.,Satoh, Yusuke,Sheffield, Justin. Spatiotemporal dynamics of global drought[J]. GEOPHYSICAL RESEARCH LETTERS,2017,44(5). |
APA | Herrera-Estrada, Julio E.,Satoh, Yusuke,&Sheffield, Justin.(2017).Spatiotemporal dynamics of global drought.GEOPHYSICAL RESEARCH LETTERS,44(5). |
MLA | Herrera-Estrada, Julio E.,et al."Spatiotemporal dynamics of global drought".GEOPHYSICAL RESEARCH LETTERS 44.5(2017). |
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