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Graph Comparing SPI and Drought Volumes 1950 - 1960
10
9
8
y = 0.0058x +2.4351
R2 = 0.6195
7
6
5
4
3
2
1
0
0
200
400
600
800
1000
Drought Volumes
Fig. 12.
Drought volumes against SPI values for Rakai.
of this research. In particular, Mr. A. W. Majugu, Principal Meteorologist
and Mr. R. Rukanyangira, Meteorologist at the Department.
Special gratitude is extended to Mr. P. Syayipuma, and Mr. W. Opio,
Water O cers Buliisa and Bujenje counties respectively, for their help dur-
ing the study in Masindi.
References
1. State of Environment Report, National Environment Management Authority
2001, Kampala Uganda, 2000.
2. L. J. Ogallo, Climatological aspects of draught. A conference on draught
mitigation, Kampala, Uganda, 1987.
3. C. P. K. Basalirwa, A paper on delineation of Uganda into climatological rain-
fall zones using the method of principal component analysis. International
Journal of Climatology 15 (1995) 1161-1177.
4. K. Subramanya, Engineering Hydrology (Mcgraw Hill-Tata, Delhi, India,
1995).
5. C. T. Haan, Statistical methods in hydrology, Iowa State University, Iowa
USA, 1983.
6. T. McKee et al ., Standardized Precipitation Index, Use in Draught Analysis
Colorado University, USA, 1993.
7. V. Yeyjevich, Tendencies in Hydrology research and its applications in
the 21st Century 1991, Water Resources Management, Vol. 5 (Springer
Netherlands), pp. 1-23.
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