Rainfall regime over the Sahelian climate gradient in the Gourma, Mali
Frédéric Frappart(1), Pierre Hiernaux(1), Françoise Guichard(2), Eric Mougin(1), Laurent Kergoat(1), Marc Arjounin(3), François Lavenu(1), Mohamed Koité(4), Jean-Emmanuel Pature(5), Thierry Lebel(3)
(1) Centre d’études spatiales de la biosphère
(CESBIO), UMR 5126 (CNES/CNRS/IRD/UPS), 18 avenue Edouard Belin, bpi
2801, 31401 Toulouse Cedex 9, France
(2) CNRM-GAME, URA 1357 (CNRS, Météo-France), 42 avenue Gaspard Coriolis, 31057, Toulouse Cedex 1, France
(3) Laboratoire d’Etude des Transferts en Hydrologie et
Environnement (LTHE), UMR 5564 (CNRS, UJF, IRD, INPG), BP 53, 38041
Grenoble Cedex 9, France
(4) Direction Nationale de la Météorologie, Bamako, Mali
(5) Université Montpellier 2 - HydroSciences Montpellier - Case
MSE - Place Eugène Bataillon, 34095 Montpellier Cedex 5, France
Abstract
The Sahelian zone is
characterized by low and variable rainfall that strongly affects the
hydrology and the climate of the region and creates severe constraints
for agriculture and water management.
This study provides a characterization of the rainfall regime in
a poorly described region of Central Sahel, Gourma (14.5° to
17.5° N and 2° to 1° S) in Mali, for the long term
precipitation daily time series during the period 1950-2007 and for a
high time resolution dataset between 2005 and 2007. First, we analyse the raingauges
data collected since the middle of the 20th century both in terms of
interannual variability and spatial distribution. Second, we
investigate the diurnal cycle of the precipitation distribution and the
nature of the rainfall using automatic raingauges during the period
2005-2007.
Gourma rainfall presents a sucession of wet (1950-1969) and dry
decades (1970-2007). The annual decrease of the rainfall is explained
by a reduction of the number of the rainy days in the South part of
Gourma and by both a decrease of the number of rainy days and of the precipitation amount per rainy day in the North and the Centre.
The results presented in this study, complete those previously reported
on other Sahelian regions located further South. The length of the
rainy season has varied since the 1950s with two episodes of short rainy season during the drought of the 1980s and since 2000 associated
to an increase in rainfall per rainy days suggesting an intensification
of the rain events.
Higher time resolution data available between 2005 and 2007,
allowed to document that most of the rainfall was produced by intense
rain events occurring mostly in the late evening and the early morning
for the core of the rainy season (July/August/September).
Keywords: Precipitation, Gourma, Sahel, interannual variability, diurnal cycle