The Standardised Precipitation-Evapotranspiration Index (SPEI) is a drought index that considers both precipitation and evapotranspiration to assess water balance conditions. It standardizes the difference between accumulated precipitation and potential evapotranspiration over a given time scale, allowing for comparisons across different climatic regions.
The SPEI is calculated by fitting the difference between cumulative precipitation and potential evapotranspiration to a probability distribution function (typically a Pearson Type III distribution) and then transforming this difference into a standardized normal variable using the inverse of the cumulative distribution function.
What is the SPEI index used for?
How does the SPEI index differ from other drought indices?
What time scales can be used for calculating the SPEI?
How is the SPEI standardized?
What does a higher SPEI value indicate?
Can the SPEI be used in any climate region?
What software tools are commonly used for calculating the SPEI?
Results are for informational purposes only and do not constitute professional advice.
