Variabilité isotopique des précipitations sahéliennes à différentes échelles de temps à Niamey (Niger) entre 1992 et 1999 : implication climatiqueIsotopic variability of Sahelian rainfall at different time steps in Niamey (Niger, 1992–1999): climatic implications |
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| Authors: | Jean-Denis Taupin Gaëlle Gaultier Guillaume Favreau Christian Leduc Christelle Marlin |
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| Institution: | 1. IRD-INAMHI, Whymper 442 y Coruña, Apartado postal 17.12.857, Quito, Ecuador;2. UMR HydroSciences Montpellier, BP 5045, 34032 Montpellier, France;3. LHGI, université Paris-11, 91405 Orsay, France |
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| Abstract: | The isotopic content of rainfall was measured in Niamey (Niger) over a period of eight years (1992–1999). Seasonal distribution of rainy events depends on the monsoon movement over the region. At the beginning and at the end of the rainy season, low rainfall, high temperatures and low relative humidity favour isotopic enrichment. In the middle of the rainy season, heavy rainfall, low temperatures and relative humidity close to saturation lead to isotopically depleted contents because of the mass effect; moreover, in the case of low rainfall, marked vertical convective development favours high altitude condensation. How far the Intertropical Front moves north, determines the quality of the rainy season and influences the isotopic contents. Thus the isotopic contents of rainfall are good climatic indicators. To cite this article: J.-D. Taupin et al., C. R. Geoscience 334 (2002) 43–50 |
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| Keywords: | Niamey Sahel rainfall isotopes climatology Niamey Sahel précipitations isotopes climatologie Géochimie Géochimie isotopique Geochemistry Isotope Geochemistry |
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