Editorial Type:
Article
Article Type:
Research Article

Computation of the Standardized Precipitation Index (SPI) and Its Use to Assess Drought Occurrences in Cameroon over Recent Decades

Guy Merlin Guenang Laboratory for Environmental Modelling and Atmospheric Physics, University of Yaoundé 1, Yaoundé, Cameroon

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F. Mkankam Kamga Laboratory for Environmental Modelling and Atmospheric Physics, University of Yaoundé 1, Yaoundé, Cameroon

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Print Publication:
01 Oct 2014
DOI:
https://doi.org/10.1175/JAMC-D-14-0032.1
Page(s):
2310–2324
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Abstract

The standardized precipitation index (SPI) is computed and analyzed using 55 years of precipitation data recorded in 24 observation stations in Cameroon along with University of East Anglia Climate Research Unit (CRU) spatialized data. Four statistical distribution functions (gamma, exponential, Weibull, and lognormal) are first fitted to data accumulated for various time scales, and the appropriate functions are selected on the basis of the Anderson–Darling goodness-of-fit statistic. For short time scales (up to 6 months) and for stations above 10°N, the gamma distribution is the most frequent choice; below this belt, the Weibull distribution predominates. For longer than 6-month time scales, there are no consistent patterns of fitted distributions. After calculating the SPI in the usual way, operational drought thresholds that are based on an objective method are determined at each station. These thresholds are useful in drought-response decision making. From SPI time series, episodes of severe and extreme droughts are identified at many stations during the study period. Moderate/severe drought occurrences are intra-annual in short time scales and interannual for long time scales (greater than 9 months), usually spanning many years. The SPI calculated from CRU gridded precipitation shows similar results, with some discrepancies at longer scales. Thus, the spatialized dataset can be used to extend such studies to a larger region—especially data-scarce areas.

Corresponding author address: G. M. Guenang, Laboratory for Environmental Modelling and Atmospheric Physics, Dept. of Physics, University of Yaoundé 1, P.O. Box 812 Yaoundé, Cameroon. E-mail: merlin.guenang@yahoo.fr

Abstract

The standardized precipitation index (SPI) is computed and analyzed using 55 years of precipitation data recorded in 24 observation stations in Cameroon along with University of East Anglia Climate Research Unit (CRU) spatialized data. Four statistical distribution functions (gamma, exponential, Weibull, and lognormal) are first fitted to data accumulated for various time scales, and the appropriate functions are selected on the basis of the Anderson–Darling goodness-of-fit statistic. For short time scales (up to 6 months) and for stations above 10°N, the gamma distribution is the most frequent choice; below this belt, the Weibull distribution predominates. For longer than 6-month time scales, there are no consistent patterns of fitted distributions. After calculating the SPI in the usual way, operational drought thresholds that are based on an objective method are determined at each station. These thresholds are useful in drought-response decision making. From SPI time series, episodes of severe and extreme droughts are identified at many stations during the study period. Moderate/severe drought occurrences are intra-annual in short time scales and interannual for long time scales (greater than 9 months), usually spanning many years. The SPI calculated from CRU gridded precipitation shows similar results, with some discrepancies at longer scales. Thus, the spatialized dataset can be used to extend such studies to a larger region—especially data-scarce areas.

Corresponding author address: G. M. Guenang, Laboratory for Environmental Modelling and Atmospheric Physics, Dept. of Physics, University of Yaoundé 1, P.O. Box 812 Yaoundé, Cameroon. E-mail: merlin.guenang@yahoo.fr
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