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Analysis of the recent evolution of dry spells in Burkina Faso

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dc.contributor.author Coulidaiti, Seraphin Palamanga Ousseini
dc.date.accessioned 2024-09-04T11:26:16Z
dc.date.available 2024-09-04T11:26:16Z
dc.date.issued 2023
dc.identifier.uri http://197.159.135.214/jspui/handle/123456789/944
dc.description A Thesis submitted to the West African Science Service Center on Climate Change and Adapted Land Use and Université Joseph KI-ZERBO, Burkina Faso in partial fulfillment of the requirements for the Master of Science Degree in Informatics for Climate Change en_US
dc.description.abstract Changes in the distribution of precipitation frequency and intensity can affect dry and wet spells, which will have an impact on climate-sensitive sectors, most notably agriculture. This study set out to analyze the variations of onset and cessation dates of the rainy season, to understand dry spells nature and their drivers in Burkina Faso. We used daily rainfall data of 10 synoptic stations from the National Meteorological Agency, the Madden-Julian Oscillation (MJO) and El Nino-Southern-Oscillation (ENSO) indices for the period 1991-2020 are then used to identify the onset and the cessation of the rainy season and their anomalies using the definitions of Sivakumar and (Kasei and Afuakwa) for season onset dates, and the definitions of Maikano and (Kasei and Afuakwa) for the season cessation dates, dry spells frequencies, longest dry spells, average dry spells duration and the modulation of the MJO and the ENSO in the occurrence of dry spells. All these parameters were computed between the onset and the cessation of the season and these dates were determined from May to October. Statistical analysis was made using Kendall's Nonparametric Test for Monotonic Trend, standard deviation, and simple linear model to assess trends in these variables. We used R programming language to extract and analyze the dry spells and the two modes, the onset and cessation dates are computed using second-order Markov chain with Instat software. We found that both changed with rainfall onsets having a more important change. The longest dry spells are identified at the cessation of the season compared with the onset of the season and there is a moderate frequency in the occurrence of DS. Across the studied period, most dry spells fluctuate between 5 and 15 days. Some phases of the MJO such as phases 5 and 7 increase the likelihood of DSs and phases 1 and 2 decrease it. At the interannual scale, the ENSO influences DS characteristics with El Nino that increase the likelihood of the DSs occurrence. To help different stakeholders with their decision-making, it would be helpful to identify the distributions and patterns of critical dry spells and explore the possibility of predicting the patterns of dry spells in the future. en_US
dc.description.sponsorship The Federal Ministry of Education and Research en_US
dc.language.iso en en_US
dc.publisher WASCAL en_US
dc.subject Dry Spell en_US
dc.subject Markov Chain en_US
dc.subject Modulation en_US
dc.subject Burkina Faso en_US
dc.subject ENSO en_US
dc.subject MJO en_US
dc.title Analysis of the recent evolution of dry spells in Burkina Faso en_US
dc.type Thesis en_US


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