Extreme rainfall events over the Pongola-Mtamvuna Water Management Area of South Africa

dc.contributor.advisorReason, Christopher
dc.contributor.advisorBlamey, Ross
dc.contributor.authorMpungose, Nomvula Bongekile
dc.date.accessioned2023-03-14T10:22:55Z
dc.date.available2023-03-14T10:22:55Z
dc.date.issued2022
dc.date.updated2023-03-14T10:21:47Z
dc.description.abstractSubtropical southern Africa experiences substantial rainfall variability both spatially and temporally, due to regional orography, geographic position, and local sea-surface temperatures. Extreme weather conditions such as droughts and floods are not uncommon and can result in both positive and negative socio-economic impacts. The Pongola-Mtamvuna Water Management Area (PM) located over north-eastern South Africa consists of communities that depend on rain-fed agriculture, as well as an inter-linked ecosystem and fresh water bodies that are dependent on rainfall. Extreme rainfall events and the systems that produce them are still not well understood, therefore, a detailed analysis of such events can contribute to an improved understanding and management of their associated risks. Here, the main focus is on the summer rainy season (October – March), rainfall variability is examined using CHIRPS daily rainfall data covering a period of thirty-seven years from 1981 – 2018. Extreme rainfall events are identified and classified for the PM area. The analysis points to the highest rainfall amounts typically occurring over low-lying coastal areas and near mountainous regions. About 60% of the extreme rainfall events were associated with tropical lows (40%) and MCS (20%). Cut-off lows (18%), cloud bands (16%), and tropical cyclones (6%) contributed to the remaining proportion. The highest frequency of events occurred during late summer months (January – March) when tropical lows and occasionally, tropical cyclones are more common. Rainfall over the PM has a statistically significant relationship with ENSO, most of the seasons with below-average rainfall and extreme events coincided with El Niño conditions. Odd cases where this was the opposite were more influenced by regional circulation anomalies which acted to enhance or reduce moisture over the land-mass thereby increasing conditions favourable/unfavourable for rainfall over the region.
dc.identifier.apacitationMpungose, N. B. (2022). <i>Extreme rainfall events over the Pongola-Mtamvuna Water Management Area of South Africa</i>. (). ,Faculty of Science ,Department of Oceanography. Retrieved from http://hdl.handle.net/11427/37429en_ZA
dc.identifier.chicagocitationMpungose, Nomvula Bongekile. <i>"Extreme rainfall events over the Pongola-Mtamvuna Water Management Area of South Africa."</i> ., ,Faculty of Science ,Department of Oceanography, 2022. http://hdl.handle.net/11427/37429en_ZA
dc.identifier.citationMpungose, N.B. 2022. Extreme rainfall events over the Pongola-Mtamvuna Water Management Area of South Africa. . ,Faculty of Science ,Department of Oceanography. http://hdl.handle.net/11427/37429en_ZA
dc.identifier.ris TY - Master Thesis AU - Mpungose, Nomvula Bongekile AB - Subtropical southern Africa experiences substantial rainfall variability both spatially and temporally, due to regional orography, geographic position, and local sea-surface temperatures. Extreme weather conditions such as droughts and floods are not uncommon and can result in both positive and negative socio-economic impacts. The Pongola-Mtamvuna Water Management Area (PM) located over north-eastern South Africa consists of communities that depend on rain-fed agriculture, as well as an inter-linked ecosystem and fresh water bodies that are dependent on rainfall. Extreme rainfall events and the systems that produce them are still not well understood, therefore, a detailed analysis of such events can contribute to an improved understanding and management of their associated risks. Here, the main focus is on the summer rainy season (October – March), rainfall variability is examined using CHIRPS daily rainfall data covering a period of thirty-seven years from 1981 – 2018. Extreme rainfall events are identified and classified for the PM area. The analysis points to the highest rainfall amounts typically occurring over low-lying coastal areas and near mountainous regions. About 60% of the extreme rainfall events were associated with tropical lows (40%) and MCS (20%). Cut-off lows (18%), cloud bands (16%), and tropical cyclones (6%) contributed to the remaining proportion. The highest frequency of events occurred during late summer months (January – March) when tropical lows and occasionally, tropical cyclones are more common. Rainfall over the PM has a statistically significant relationship with ENSO, most of the seasons with below-average rainfall and extreme events coincided with El Niño conditions. Odd cases where this was the opposite were more influenced by regional circulation anomalies which acted to enhance or reduce moisture over the land-mass thereby increasing conditions favourable/unfavourable for rainfall over the region. DA - 2022_ DB - OpenUCT DP - University of Cape Town KW - Ocean and Atmosphere Science LK - https://open.uct.ac.za PY - 2022 T1 - Extreme rainfall events over the Pongola-Mtamvuna Water Management Area of South Africa TI - Extreme rainfall events over the Pongola-Mtamvuna Water Management Area of South Africa UR - http://hdl.handle.net/11427/37429 ER - en_ZA
dc.identifier.urihttp://hdl.handle.net/11427/37429
dc.identifier.vancouvercitationMpungose NB. Extreme rainfall events over the Pongola-Mtamvuna Water Management Area of South Africa. []. ,Faculty of Science ,Department of Oceanography, 2022 [cited yyyy month dd]. Available from: http://hdl.handle.net/11427/37429en_ZA
dc.language.rfc3066eng
dc.publisher.departmentDepartment of Oceanography
dc.publisher.facultyFaculty of Science
dc.subjectOcean and Atmosphere Science
dc.titleExtreme rainfall events over the Pongola-Mtamvuna Water Management Area of South Africa
dc.typeMaster Thesis
dc.type.qualificationlevelMasters
dc.type.qualificationlevelMSc
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