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Índice Padronizado de Precipitação e Evapotranspiração×NDVI×
ÁreaGeofísicaGeofísica
FamíliaProcess / pipelineProcess / pipeline
Ano de origem20101973
Autor originalVicente-Serrano, Beguería, and López-MorenoRouse, Haas, Schell, and Deering
TipoProbability-based water deficit indicatorSpectral index for vegetation assessment
Fonte seminalVicente-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 ↗Rouse, J. W., Haas, R. H., Schell, J. A., & Deering, D. W. (1973). Monitoring vegetation systems in the Great Plains with ERTS. Third Earth Resources Technology Satellite Symposium Proceedings, 1, 309-317. link ↗
Outros nomesSPEINDVI
Relacionados33
ResumoThe 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.The Normalized Difference Vegetation Index (NDVI) is a spectral index computed from satellite or aerial multispectral imagery that quantifies vegetation greenness and vigor. Introduced by Rouse and colleagues in 1973 using Landsat data, NDVI has become the most widely used remote sensing metric for vegetation monitoring, drought assessment, crop productivity forecasting, and land cover change detection.
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ScholarGateComparar métodos: Standardized Precipitation Evapotranspiration Index · NDVI. Recuperado em 2026-06-19 de https://scholargate.app/pt/compare