The Response of Geopotential Height Anomalies to El Niño and La Niña Conditions and Their Implications to Seasonal Rainfall Variability over the Horn of Africa

Abstract

In this study, we unveil atmospheric circulation anomalies associated with t he large-scale tropical teleconnections using National Center for Environmental Prediction (NCEP) reanalysis dataset. Composite analyses have been performed to know the impact of large-scale tropical circulations on the Horn of Africa. The composite analysis performed at the geopotential height of 850 Mb and 200 Mb, and precipitation rate (mm/day) during six strong El Ni ñ o and La Ni ñ a episodes revealed that the large-scale tropical variability induc ed climate anomalies in space and time. A substantial decrease in upper-level height (200 Mb) has been observed in the study area during El Ni ñ o composite years as compared to the La Ni ñ a years. During El Ni ñ o conditions, the upper-level divergence initiates low-level vertical motion, thereby enhancing convection, however, during La Ni ñ a composite years, nearly contrasting situations are noticed in Belg (February to May) season in Ethiopia. However, geopotential height anomalies at 850 Mb are above-normal during the strong El Ni ñ o years, suggesting suppressed convection due to vertical shrinking and enhancement of divergence at the lower level. Compared to the Belg (February to May), geopotential anomalies were generally positive during the Kiremt (June to September) season, thereby suppressing the rainfall, particularly in Southern Ethiopia and Northern Part of Kenya. In contrast, an increase in rainfall was observed during the Belg season (February to May).