The Role of the Dominant Modes of Precipitation Variability over Eastern Africa in Modulating the Hydrology of Lake Victoria

Table 1

Regressions of rainfall for 1956–1990. is catchment rainfall; is lake rainfall (from Tate).

Catchment	Regression	Correlation,
Nzoia	= (0.685  *  ) + 154.5	0.54
Yala	= (0.951  *  ) + 64.7	0.61
Sondu	= (0.666  *  ) + 302.6	0.39
Awach Kaboun	= (0.785  *  ) + 337.4	0.28
Kagera	= (0.556  *  ) + 142.8	0.60