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dc.contributor.authorWeiss, Jeremy L.
dc.contributor.authorCastro, Christopher L.
dc.contributor.authorOverpeck, Jonathan T.
dc.date.accessioned2025-03-06T17:16:53Z
dc.date.available2025-03-06T17:16:53Z
dc.date.issued2009-11-15
dc.identifier.citationWeiss, J. L., C. L. Castro, and J. T. Overpeck, 2009: Distinguishing Pronounced Droughts in the Southwestern United States: Seasonality and Effects of Warmer Temperatures. J. Climate, 22, 5918–5932, https://doi.org/10.1175/2009JCLI2905.1.en_US
dc.identifier.issn0894-8755
dc.identifier.doi10.1175/2009jcli2905.1
dc.identifier.urihttp://hdl.handle.net/10150/676864
dc.description.abstractHigher temperatures increase the moisture-holding capacity of the atmosphere and can lead to greater atmospheric demand for evapotranspiration, especially during warmer seasons of the year. Increases in precipitation or atmospheric humidity ameliorate this enhanced demand, whereas decreases exacerbate it. In the southwestern United States (Southwest), this means the greatest changes in evapotranspirational demand resulting from higher temperatures could occur during the hot–dry foresummer and hot–wet monsoon. Here seasonal differences in surface climate observations are examined to determine how temperature and moisture conditions affected evapotranspirational demand during the pronounced Southwest droughts of the 1950s and 2000s, the latter likely influenced by warmer temperatures now attributed mostly to the buildup of greenhouse gases. In the hot–dry foresummer during the 2000s drought, much of the Southwest experienced significantly warmer temperatures that largely drove greater evapotranspirational demand. Lower atmospheric humidity at this time of year over parts of the region also allowed evapotranspirational demand to increase. Significantly warmer temperatures in the hot–wet monsoon during the more recent drought also primarily drove greater evapotranspirational demand, but only for parts of the region outside of the core North American monsoon area. Had atmospheric humidity during the more recent drought been as low as during the 1950s drought in the core North American monsoon area at this time of year, greater evapotranspirational demand during the 2000s drought could have been more spatially extensive. With projections of future climate indicating continued warming in the region, evapotranspirational demand during the hot–dry and hot–wet seasons possibly will be more severe in future droughts and result in more extreme conditions in the Southwest, a disproportionate amount negatively impacting society.en_US
dc.language.isoenen_US
dc.publisherAmerican Meteorological Societyen_US
dc.rights© 2009 American Meteorological Society.en_US
dc.rights.urihttp://rightsstatements.org/vocab/InC/1.0/en_US
dc.subjectDroughten_US
dc.subjectSeasonal effectsen_US
dc.subjectEvapotranspirationen_US
dc.subjectPrecipitationen_US
dc.titleDistinguishing Pronounced Droughts in the Southwestern United States: Seasonality and Effects of Warmer Temperaturesen_US
dc.typeArticleen_US
dc.identifier.eissn1520-0442
dc.contributor.departmentDepartment of Geosciences, The University of Arizonaen_US
dc.contributor.departmentDepartment of Atmospheric Sciences, The University of Arizonaen_US
dc.contributor.departmentInstitute of the Environment, The University of Arizonaen_US
dc.identifier.journalJournal of Climateen_US
dc.description.note6 month embargoen_US
dc.description.collectioninformationThis item from the UA Faculty Publications collection is made available by the University of Arizona with support from the University of Arizona Libraries. If you have questions, please contact us at repository@u.library.arizona.edu.en_US
dc.eprint.versionFinal published versionen_US
dc.source.journaltitleJournal of Climate
dc.source.volume22
dc.source.issue22
dc.source.beginpage5918
dc.source.endpage5932
refterms.dateFOA2025-03-06T17:16:57Z


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