Please use this identifier to cite or link to this item: http://hdl.handle.net/10397/100705
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dc.contributorDepartment of Land Surveying and Geo-Informaticsen_US
dc.creatorZhang, Ben_US
dc.creatorWang, Sen_US
dc.creatorWang, Yen_US
dc.date.accessioned2023-08-11T03:12:48Z-
dc.date.available2023-08-11T03:12:48Z-
dc.identifier.issn2169-897Xen_US
dc.identifier.urihttp://hdl.handle.net/10397/100705-
dc.language.isoenen_US
dc.publisherWiley-Blackwellen_US
dc.rights©2019. American Geophysical Union. All Rights Reserved.en_US
dc.titleCopula‐based convection‐permitting projections of future changes in multivariate drought characteristicsen_US
dc.typeJournal/Magazine Articleen_US
dc.identifier.spage7460en_US
dc.identifier.epage7483en_US
dc.identifier.volume124en_US
dc.identifier.issue14en_US
dc.identifier.doi10.1029/2019JD030686en_US
dcterms.abstractProbabilistic projections of future drought characteristics play a crucial role in climate change adaptation and disaster risk reduction. This study presents a copula-based probabilistic framework for projecting future changes in multivariable drought characteristics through convection-permitting Weather Research and Forecasting simulations with 4-km horizontal grid spacing. A probabilistic multivariate drought index is introduced to examine the joint effects of drought indicators with uncertainty intervals for four major river basins located in South Central Texas of the United States. Markov chain Monte Carlo is used to address uncertainties in assessing copula parameters and in predicting climate-induced changes in hydrological regimes. Our findings reveal that the severity and intensity of drought episodes can be amplified when considering the compound effects of soil moisture and runoff regimes by using the probabilistic multivariate drought index. The South Central Texas region is projected to experience more drought events with shorter duration and higher intensity in a changing climate. The drought severity will not necessarily increase due to the decreasing drought duration. In addition, our findings indicate that the intensity of future droughts is expected to increase as a result of the deficiency of soil moisture even though precipitation extremes are projected to become more frequent. Moreover, climate change impacts on multivariate drought characteristics will intensify with the increasing temporal scales (i.e., short-, medium-, and long-term droughts) although the number of future drought events may decrease by the end of this century.en_US
dcterms.accessRightsopen accessen_US
dcterms.bibliographicCitationJournal of geophysical research. Atmospheres, 27 July 2019, v. 124, no. 14, p. 7460-7483en_US
dcterms.isPartOfJournal of geophysical research. Atmospheresen_US
dcterms.issued2019-07-27-
dc.identifier.scopus2-s2.0-85068606282-
dc.identifier.eissn2169-8996en_US
dc.description.validate202305 bckwen_US
dc.description.oaVersion of Recorden_US
dc.identifier.FolderNumberLSGI-0191-
dc.description.fundingSourceOthersen_US
dc.description.fundingTextNational Natural Science Foundation of China; Hong Kong Polytechnic University Start-up Granten_US
dc.description.pubStatusPublisheden_US
dc.identifier.OPUS28572877-
dc.description.oaCategoryVoR alloweden_US
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