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dc.contributor.authorTRAORE Vieux Boukhaly-
dc.contributor.authorDIOUF Rokhaya-
dc.contributor.authorNDIAYE Mamadou Lamine-
dc.contributor.authorGODFROYD Ousman Rilengar-
dc.contributor.authorFAYE Moustapha-
dc.contributor.authorMALOMAR Giovani-
dc.contributor.authorSARR Joseph-
dc.contributor.authorDIAW Amadou Tahirou-
dc.contributor.authorBEYE Aboubaker Chedikh-
dc.date.accessioned2018-06-
dc.date.available2018-06-
dc.date.issued2018-06-
dc.identifier.issn2170-1318-
dc.identifier.urihttp://dspace.univ-ouargla.dz/jspui/handle/123456789/19244-
dc.descriptionAlgerian Journal of Arid And Environment (AJAE)en_US
dc.description.abstractAnnual rainfall data used in this study was provided by National Agency of Civil Aviation and Meteorology measured in 14 stations of 14 regions of Senegal. Standard normal homogeneity test was performed on these data to detect possible climatic accidents. Our main goal was to provide national decision-makers with plausible scenarios of climate change for all regions of the country. It is to equip them to: i) adapt their natural resource management strategies to climate change issues; and ii) strengthen the scientific base for their own benefit. For all 14 stations, the null hypothesis of no break is rejected at the 5% threshold and the break dates are between 1955 and 1971 depending on the region. The comparison of averages across the breaking point shows that this break is down for all 14 stations. The characterization of the mean amplitudes before and after rupture shows that this decrease did not have the same intensity in the 14 regions. Finally, the characterization of the wet and dry sequences shows that the temporal persistence of the drought is not at the same level for the 14 regions. In conclusion, the statistical analysis of the rainfall contributions confirms the dissymmetry and the general downward trend and therefore the low water level in Senegal. Such results suggest the need for water authorities to formulate effective water management policies according to the prevailing and future climatic conditions. Transitional, adaptive and urgent measures may be undertaken by priority according regions.en_US
dc.language.isofren_US
dc.relation.ispartofseriesvolume 8 numéro 1 2018;-
dc.subjectHomogeneity analysisen_US
dc.subjectbreak pointsen_US
dc.subjectdroughts eventsen_US
dc.subjectclimate changeen_US
dc.subjectwater availabilityen_US
dc.subjectsustainable developmenten_US
dc.subjectfood securityen_US
dc.subjectagricultural policyen_US
dc.titleDETECTION OF INHOMOGENEITIES AND BREAK POINTS IN ANNUAL RAINFALL SERIES OF SENEGALREGIONSen_US
dc.typeArticleen_US
Appears in Collections:volume 08 numéro 1 2018

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