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    Distinguishing Pronounced Droughts in the Southwestern United States: Seasonality and Effects of Warmer Temperatures

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    clim-2009jcli2905.1.pdf
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    Author
    Weiss, Jeremy L.
    Castro, Christopher L.
    Overpeck, Jonathan T. cc
    Affiliation
    Department of Geosciences, The University of Arizona
    Department of Atmospheric Sciences, The University of Arizona
    Institute of the Environment, The University of Arizona
    Issue Date
    2009-11-15
    Keywords
    Drought
    Seasonal effects
    Evapotranspiration
    Precipitation
    
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    Citation
    Weiss, 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.
    Publisher
    American Meteorological Society
    Journal
    Journal of Climate
    URI
    http://hdl.handle.net/10150/676864
    DOI
    10.1175/2009jcli2905.1
    Abstract
    Higher 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.
    Type
    Article
    Language
    en
    ISSN
    0894-8755
    EISSN
    1520-0442
    ae974a485f413a2113503eed53cd6c53
    10.1175/2009jcli2905.1
    Scopus Count
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    CLIMAS Publications
    UA Faculty Publications

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