Statistical Analysis of Recent and Future Rainfall

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dc.contributor.authorLawin, Agnidé Emmanuel
dc.contributor.authorHounguè, Nina Rholan
dc.contributor.authorBiaou, Angelbert Chabi
dc.contributor.authorBadou, Djigbo Félicien
dc.date.accessioned2022-04-13T12:11:48Z
dc.date.available2022-04-13T12:11:48Z
dc.date.issued2019-01-06
dc.descriptionModifications in the climate as a result of both natural and anthropogenic processes have raised considerable concerns (such as more frequent and intense rainfall, droughts, dry spells, violent winds, etc.), as they induce adverse impacts on several development sectors. In recent decades, weather and climate extremes such as droughts, heat waves, wild fires, floods and storms have increased in frequency and intensity in several regions of the world. In fact, Vincent et al. noticed that the percentage of warm nights is increasing while that of cold nights is decreasing in South-America. In addition, the US Climate Change Science Program underscored the fact that heavy precipitations have become more frequent and intense in Northern America. In central Asia, Savitskaya reported that, during the last 50 years, there was high variability in the pattern of precipitation, whereas winter has become warmer in the entire region.en_US
dc.description.abstractThis paper assessed the current and mid-century trends in rainfall and temperature over the Mono River watershed. It considered observation data for the period 1981–2010 and projection data from the regional climate model (RCM), REMO, for the period 2018–2050 under emission scenarios RCP4.5 and RCP8.5. Rainfall data were interpolated using ordinary kriging. Mann-Kendall, Pettitt and Standardized Normal Homogeneity (SNH) tests were used for trends and break-points detection. Rainfall interannual variability analysis was based on standardized precipitation index (SPI), whereas anomalies indices were considered for temperature. Results revealed that on an annual scale and all over the watershed, temperature and rainfall showed an increasing trend during the observation period. By 2050, both scenarios projected an increase in temperature compared to the baseline period 1981–2010, whereas annual rainfall will be characterized by high variabilities. Rainfall seasonal cycle is expected to change in the watershed: In the south, the second rainfall peak, which usually occurs in September, will be extended to October with a higher value. In the central and northern parts, rainfall regime is projected to be characterized by late onsets, a peak in September and lower precipitation until June and higher thereafter. The highest increase and decrease in monthly precipitation are expected in the northern part of the watershed. Therefore, identifying relevant adaptation strategies is recommended.en_US
dc.description.sponsorshipThee West African Science Service Center for Climate Change and Adapted Land use (WASCAL). World Bank.en_US
dc.identifier.urihttp://hdl.handle.net/123456789/1390
dc.language.isoenen_US
dc.publisherResearch Gateen_US
dc.relation.ispartofseriesDOI: 10.3390/cli7010008;17
dc.subjectMono River watersheden_US
dc.subjecttrend analysisen_US
dc.subjectclimateen_US
dc.titleStatistical Analysis of Recent and Future Rainfallen_US
dc.typeArticleen_US
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