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Standardized Precipitation Evapotranspiration Index

The Standardized Precipitation Evapotranspiration Index (SPEI) is a climate index that combines precipitation and temperature (via reference evapotranspiration) to characterize water deficits and droughts. Developed by Vicente-Serrano and colleagues in 2010, SPEI extends the SPI framework to account for the combined effect of precipitation deficiency and increased evaporative demand from warming, providing a more physically-based drought metric than precipitation-only indices.

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Vicente-Serrano, S. M., Beguería, S., & López-Moreno, J. I. (2010). A multiscalar drought index sensitive to global warming: the Standardized Precipitation Evapotranspiration Index. Journal of Climate, 23(7), 1696-1718. · DOI 10.1175/2009JCLI2909.1

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Same method familyGeneral Circulation Modelmachine-suggested · Relational suggestion, not evidence.Same method familyNDVImachine-suggested · Relational suggestion, not evidence.Same method familyStandardized Precipitation Indexmachine-suggested · Relational suggestion, not evidence.