Abstract

This study focused on the customization of the fourth generation International Center for Theoretical Physics Regional Climate Model version 4.4 and its ability to reproduce the mean climate and most dominant modes of variability over East Africa. The simulations were performed at a spatial resolution of 25 km for the period 1998–2013. The model was driven by ERA-Interim reanalysis. The customization focus was on cumulus and microphysics schemes during the Short Rains for the year 2000. The best physics combinations were then utilized for the validation studies. The East Africa region and Lake Victoria Basin region are adapted to carry out empirical orthogonal function analysis, during the Short and Long Rains. Tropical Rainfall Measuring Mission data was utilized in the validation of the model. The first mode of variability from the model and observational data during the Short Rains was associated with the warming of the Pacific Ocean and the sea surface temperature gradients over the Indian Ocean. During the Long rains, the inter-annual rainfall variability over the Lake Victoria region was associated with the sea surface temperature anomaly over the Indian Ocean and for the East Africa region the associations were weak. The drivers during the Long Rains over East Africa region were then further investigated by splitting the season to the March–April and May periods. The March–April period was positively correlated to the West Pacific and Indian Ocean dipole index, while May was associated with the Quasi-Biennial Oscillation. In conclusion, although the model can reproduce the dominant modes of variability as in the observational data sets during the Short Rains, skill was lower during the Long Rains.

Highlights

  • The recent advancement of computational power has allowed various climate modeling groups worldwide to utilize Regional Climate Models (RCMs)

  • The simulations utilizing Grell schemes underestimate total precipitation, the different closure assumptions account for the different precipitation amounts, Grell AS releases buoyant energy every time step while the Grell FC closure dissipates the buoyant energy at time scales that are approximately half an hour [57]

  • Long Rains utilizing the East Africa domain and the Lake Victoria Basin with the results described

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Summary

Introduction

The recent advancement of computational power has allowed various climate modeling groups worldwide to utilize Regional Climate Models (RCMs). The use of Regional Climate Models has been on the rise worldwide, a relatively limited number of studies have been conducted over. The region has experienced numerous devastating droughts [2,3,4]. The droughts have undoubtedly caused social-economic disruption of livelihoods in the region [5] and further deterioration of the ecosystem [6,7]. Rainfall over East Africa exhibits a bimodal pattern, caused by the North-South migration of the Intertropical Convergence Zone (ITCZ). The Long Rains (March to May) are less variable and receive higher rainfall amounts compared to the Short Rains (October to December) [8]. Studies on inter-annual variability of precipitation over East Africa identified El

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