ENSO and interannual rainfall variability in Uganda: Implications for agricultural management

The El Nino-Southern Oscillation (ENSO) is correlated with the short rainy season (September-December) in East Africa. Seasonal climate forecasts made on this basis are being disseminated in the hope that this information wil l be useful in regional or even local planning and resource management. In order to improve the likelihood of success in using regional forecasts in U ganda, particularly in the agricultural sector, climate analysis was perfor med at the sub-regional level with distinctions being made between unimodal (short season peak in August) and bimodal (short season peak in November) rainfall zones. Monthly climate data from 1931 to 1960 were available for 3 3 sites. Averaging across all stations, it is shown that Pacific Ocean NINO 3 region sea-surface temperatures (SSTs) from July to September (JAS) are s ignificantly correlated with both the concurrent August-September (AS) rain fall (r = -0.75) and the following November-December (ND) rainfall (r = 0.5 7), but with opposite signs. When station data are separated into uni- and bimodal sites, it becomes clear that the importance of ENSO events is diffe rent in the two zones. In the unimodal zone, El Nino events are associated with a depression of the August peak in rainfall, but a lengthening of the season, potentially providing an opportunity for growing later-maturing cro ps. At bimodal sites, there is very little impact in August but November ra infall is enhanced in El Nino years and depressed in La Nina years. Given a forecast of ENSO, the primary strategies that will be useful in farm manag ement will differ by rainfall zone and will revolve around the choice of cr op or cultivar and the timing of planting in order to make optimal use of t he growing period. Copyright (C) 2000 Royal Meteorological Society.