Knowledge Resource Center for Ecological Environment in Arid Area
DOI | 10.1029/2020WR027755 |
Drought Propagation in Contiguous US Watersheds: A Process-Based Understanding of the Role of Climate and Watershed Properties | |
Apurv, Tushar; Cai, Ximing | |
通讯作者 | Cai, XM |
来源期刊 | WATER RESOURCES RESEARCH
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ISSN | 0043-1397 |
EISSN | 1944-7973 |
出版年 | 2020 |
卷号 | 56期号:9 |
英文摘要 | Drought impacts on the society and environment are influenced by how droughts propagate through the hydrologic cycle; however, the physical processes involved in drought propagation are not well understood. In this study, a physically based hydrologic model is used to understand the drought propagation mechanisms and their controlling factors in multiple watersheds selected from different regions of the contiguous United States (CONUS). The characteristics of hydrologic droughts are found to be significantly different in three regions of the CONUS: (1) western U.S. watersheds have long and intense streamflow droughts, (2) Great Plains and southwest U.S. watersheds have low intensity and duration of streamflow droughts, and (3) eastern U.S. watersheds have short but intense streamflow droughts. This spatial pattern of hydrologic drought characteristics is found to coincide with the pattern of climate properties. Highly seasonal recharge driven by winter precipitation or snowmelt leads to longer streamflow droughts in the western United States; whereas humid climate with low seasonality in the eastern United States leads to shorter streamflow droughts. Furthermore, the storage-discharge relationship is identified as a key watershed property which controls the intensity of hydrologic droughts. Higher sensitivity of baseflow to watershed storage in the western and the eastern U.S. watersheds leads to more intense streamflow droughts in these regions. In the Great Plains and southwest United States, watersheds have a lower sensitivity of baseflow to catchment storage which, combined with the highly arid climate, leads to low variability in baseflow, and in turn results in low intensity of streamflow droughts in the region. |
英文关键词 | drought propagation hydrologic processes storage-discharge relationship seasonality aridity |
类型 | Article |
语种 | 英语 |
收录类别 | SCI-E |
WOS记录号 | WOS:000578452200054 |
WOS关键词 | METEOROLOGICAL DROUGHT ; HYDROLOGICAL DROUGHTS ; CATCHMENT ; INDEX ; FLOW ; SENSITIVITY ; RECESSION ; RAINFALL ; SCALE ; VULNERABILITY |
WOS类目 | Environmental Sciences ; Limnology ; Water Resources |
WOS研究方向 | Environmental Sciences & Ecology ; Marine & Freshwater Biology ; Water Resources |
资源类型 | 期刊论文 |
条目标识符 | http://119.78.100.177/qdio/handle/2XILL650/326794 |
作者单位 | [Apurv, Tushar; Cai, Ximing] Univ Illinois, Dept Civil & Environm Engn, VenTe Chow Hydrosyst Lab, Urbana, IL 61820 USA |
推荐引用方式 GB/T 7714 | Apurv, Tushar,Cai, Ximing. Drought Propagation in Contiguous US Watersheds: A Process-Based Understanding of the Role of Climate and Watershed Properties[J],2020,56(9). |
APA | Apurv, Tushar,&Cai, Ximing.(2020).Drought Propagation in Contiguous US Watersheds: A Process-Based Understanding of the Role of Climate and Watershed Properties.WATER RESOURCES RESEARCH,56(9). |
MLA | Apurv, Tushar,et al."Drought Propagation in Contiguous US Watersheds: A Process-Based Understanding of the Role of Climate and Watershed Properties".WATER RESOURCES RESEARCH 56.9(2020). |
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