4.2 Article

Influence of spatial and temporal scales on statistical analyses of rainfall variability in the River Nile basin

Journal

DYNAMICS OF ATMOSPHERES AND OCEANS
Volume 77, Issue -, Pages 26-42

Publisher

ELSEVIER
DOI: 10.1016/j.dynatmoce.2016.10.008

Keywords

Empirical orthogonal function (EOF); Variability analyses; River Nile basin; Climate variability; Rainfall variability; Meteorology

Funding

  1. IRO Ph.D. scholarship of KU Leuven

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In this study, empirical orthogonal function was applied to analyze rainfall variability in the Nile basin based on various spatio-temporal scales. The co-occurrence of rainfall variability and the Variation in selected climate indices was analyzed based on various spatio-temporal scales. From the highest to the lowest, the cumulative amount of variance explained by the first two principal components (PCs) for any selected size of the spatial domain was obtained for the annual, seasonal, and monthly rainfall series respectively. The variability in the annual rainfall of 1 degrees x 1 degrees spatial coverage explained by only the first PC was about 55% on average. However, this percentage reduced to about 40% on average across the study area when the size of the spatial domain was increased from 1 degrees x 1 degrees to 10 degrees x 10 degrees. The variation in climate indices was shown to explain rainfall variability more suitably at a regional than location-specific spatial scale. The magnitudes and sometimes signs of the correlation between rainfall variability and the variation in climate indices tended to vary from one time scale to another. These findings are vital in the selection of spatial and temporal scales for more considered attribution of rainfall variability across the study area. (C) 2016 Elsevier B.V. All rights reserved.

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