Computation of Drought Index SPI with Alternative Distribution Functions
The Standardized Precipitation Index (SPI) is widely used as drought meteorological index, to identify the duration and/or severity of a drought. The SPI is usually computed by fitting the gamma probability distribution to the observed precipitation data. In this work, the possibility to calculate S...
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Veröffentlicht in: | Water resources management 2012-07, Vol.26 (9), p.2453-2473 |
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