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. 2017 Sep 25;14(10):1119. doi: 10.3390/ijerph14101119

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© 2017 by the authors.

Licensee MDPI, Basel, Switzerland. This article is an open access article distributed under the terms and conditions of the Creative Commons Attribution (CC BY) license (http://creativecommons.org/licenses/by/4.0/).

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Upper panel: (a) variation of EIR as a function of rainfall by averaged Senegal zones (North, central, and South. Lower panel: (b) variation of EIR as a function of temperature by averaged Senegal zones (North, central, and South). The rainfall is from CHIRPS, and the temperature is derived from different reanalysis data. Simulated EIR are shown for the common period 1981–2001.

Upper panel: (a) variation of EIR as a function of rainfall by averaged Senegal zones (North, central, and South. Lower panel: (b) variation of EIR as a function of temperature by averaged Senegal zones (North, central, and South). The rainfall is from CHIRPS, and the temperature is derived from different reanalysis data. Simulated EIR are shown for the common period 1981–2001.