4.6 Article

Influence of topography on rainfall variability in Santiago Island, Cape Verde

Journal

INTERNATIONAL JOURNAL OF CLIMATOLOGY
Volume 34, Issue 4, Pages 1081-1097

Publisher

WILEY-BLACKWELL
DOI: 10.1002/joc.3747

Keywords

rainfall variability; rainfall parametrization; topography; multiple regression analysis; kriging; Cape Verde; long-term rainfall

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Cape Verde is a semi-arid country conformed by a group of islands located off the west coast of Africa, with highly variable rainfall that appears during a single rainy season. Santiago Island, the biggest of the country, is characterized for abrupt changes of relief within small distances. The influence of geographic location and topographic parameters, such as slope gradient, exposition and elevation on the variability of rainfall in Santiago Island was studied using monthly rainfall data of 30 seasons (1981 to 2010), with daily rainfall data for 14 seasons (1997 to 2010). The number of rainfall days and the percentage of maximum daily rainfall within the monthly and seasonal totals were evaluated. Few rainy days can control the monthly and seasonal rainfall patterns of Santiago Island. Multivariate linear regressions among daily, monthly and seasonal rainfall and elevation, slope gradient, aspect, and geographic east and west coordinates as predictors were carried out. Elevation explains most of the variance in the rainfall. The coefficients of determination show an inverse relationship with the rainfall depth: moderate rainfall totals (120-150mm monthly, 250-300mm seasonal) produced the best correlations for seasonal and monthly rainfall, while very low (<50mm for monthly, <200mm for seasonal) and very high amounts (>250mm for monthly, >350mm for seasonal) resulted in poor correlations. Long-term mean rainfall was interpolated using ordinary kriging and kriging with external drift. In Santiago Island, high and more extreme rainfall events are less influenced by elevation, while low and medium rainfall events are significantly influenced by orography, with most of the rainfall appearing on high elevations. Copyright (c) 2013 Royal Meteorological Society

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