Projections of extreme rainfall in South Africa using CMIP6 ISIMIP models.
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| Title: | Projections of extreme rainfall in South Africa using CMIP6 ISIMIP models. |
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| Authors: | Mohomi, Tumelo1,2 (AUTHOR) mohomitumelo@icloud.com, Stepanenko, Victor3,4,5 (AUTHOR) v.stepanenko@rcc.msu.ru, Medvedev, Alexander3,4,5 (AUTHOR) a.medvedev@rcc.msu.ru, Dhau, Inos1 (AUTHOR) inos.dhau@ul.ac.za, Chikoore, Hector1,6 (AUTHOR) hector.chikoore@ul.ac.za, Bopape, Mary-Jane7,8 (AUTHOR) mm.bopape@saeon.nrf.ac.za |
| Source: | Climate Dynamics. Mar2026, Vol. 64 Issue 3, p1-29. 29p. |
| Abstract: | The escalating impacts of climate change pose a significant risk to South Africa’s water resources and infrastructure, particularly as a result of increased frequency and intensity of extreme rainfall. This study presents extreme rainfall projections for the country by analysing Phase 6 of the Coupled Model Intercomparison Project (CMIP6) Inter-Sectoral Impact Model Intercomparison Project (ISIMIP) global climate models (GCMs) from 2020 to 2100, under SSP1-2.6 and SSP5-8.5 scenarios. Five models and their ensembles were evaluated against ECMWF ERA5-Land and station data using Taylor diagrams, NSE, RMSE, PBIAS, and R². The ensemble outperformed individual models, which showed a similar spatial bias, underestimating rainfall over the escarpment while overestimating it in the lowlands. Rainfall changes were analysed for the near- (2020–2055) and far-future (2065–2100), focusing on the 5th, 50th, and 95th percentiles. Future midlatitude and subtropical circulation changes were projected to intensify the west-east rainfall gradient, leading to a drier west and a wetter east. This trend drives an overall increase in extreme rainfall events across South Africa. Annually, this is reflected in drier conditions projected along the coast and northeast in the far-future (5th and 50th percentiles), while the eastern half will likely experience increased extreme wet conditions (95th percentile). January projects rainfall increases in the eastern interior, with extreme wet conditions increasing by 35–45 mm across scenarios. Conversely, October may experience increased extreme dry conditions (5th percentile), with more than 48 mm decrease in the far-future under SSP5-8.5. During austral summer (DJF), pronounced wet and dry extremes are projected over eastern South Africa. Austral winter (JJA) will likely experience persistent and intensifying dry and wet extremes along the coast, with the southwest Cape particularly vulnerable to severe dry conditions. Heavy rainfall days are projected to increase in eastern South Africa, exceeding 10 days in the eastern interior. This study is crucial for understanding rainfall extremes under a changing atmospheric circulation and unpins more effective climate change adaptation strategies in South Africa. [ABSTRACT FROM AUTHOR] |
| Copyright of Climate Dynamics is the property of Springer Nature and its content may not be copied or emailed to multiple sites without the copyright holder's express written permission. Additionally, content may not be used with any artificial intelligence tools or machine learning technologies. However, users may print, download, or email articles for individual use. This abstract may be abridged. No warranty is given about the accuracy of the copy. Users should refer to the original published version of the material for the full abstract. (Copyright applies to all Abstracts.) | |
| Database: | Engineering Source |
| FullText | Text: Availability: 0 |
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| Header | DbId: egs DbLabel: Engineering Source An: 192064573 AccessLevel: 6 PubType: Academic Journal PubTypeId: academicJournal PreciseRelevancyScore: 0 |
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| Items | – Name: Title Label: Title Group: Ti Data: Projections of extreme rainfall in South Africa using CMIP6 ISIMIP models. – Name: Author Label: Authors Group: Au Data: <searchLink fieldCode="AR" term="%22Mohomi%2C+Tumelo%22">Mohomi, Tumelo</searchLink><relatesTo>1,2</relatesTo> (AUTHOR)<i> mohomitumelo@icloud.com</i><br /><searchLink fieldCode="AR" term="%22Stepanenko%2C+Victor%22">Stepanenko, Victor</searchLink><relatesTo>3,4,5</relatesTo> (AUTHOR)<i> v.stepanenko@rcc.msu.ru</i><br /><searchLink fieldCode="AR" term="%22Medvedev%2C+Alexander%22">Medvedev, Alexander</searchLink><relatesTo>3,4,5</relatesTo> (AUTHOR)<i> a.medvedev@rcc.msu.ru</i><br /><searchLink fieldCode="AR" term="%22Dhau%2C+Inos%22">Dhau, Inos</searchLink><relatesTo>1</relatesTo> (AUTHOR)<i> inos.dhau@ul.ac.za</i><br /><searchLink fieldCode="AR" term="%22Chikoore%2C+Hector%22">Chikoore, Hector</searchLink><relatesTo>1,6</relatesTo> (AUTHOR)<i> hector.chikoore@ul.ac.za</i><br /><searchLink fieldCode="AR" term="%22Bopape%2C+Mary-Jane%22">Bopape, Mary-Jane</searchLink><relatesTo>7,8</relatesTo> (AUTHOR)<i> mm.bopape@saeon.nrf.ac.za</i> – Name: TitleSource Label: Source Group: Src Data: <searchLink fieldCode="JN" term="%22Climate+Dynamics%22">Climate Dynamics</searchLink>. Mar2026, Vol. 64 Issue 3, p1-29. 29p. – Name: Abstract Label: Abstract Group: Ab Data: The escalating impacts of climate change pose a significant risk to South Africa’s water resources and infrastructure, particularly as a result of increased frequency and intensity of extreme rainfall. This study presents extreme rainfall projections for the country by analysing Phase 6 of the Coupled Model Intercomparison Project (CMIP6) Inter-Sectoral Impact Model Intercomparison Project (ISIMIP) global climate models (GCMs) from 2020 to 2100, under SSP1-2.6 and SSP5-8.5 scenarios. Five models and their ensembles were evaluated against ECMWF ERA5-Land and station data using Taylor diagrams, NSE, RMSE, PBIAS, and R². The ensemble outperformed individual models, which showed a similar spatial bias, underestimating rainfall over the escarpment while overestimating it in the lowlands. Rainfall changes were analysed for the near- (2020–2055) and far-future (2065–2100), focusing on the 5th, 50th, and 95th percentiles. Future midlatitude and subtropical circulation changes were projected to intensify the west-east rainfall gradient, leading to a drier west and a wetter east. This trend drives an overall increase in extreme rainfall events across South Africa. Annually, this is reflected in drier conditions projected along the coast and northeast in the far-future (5th and 50th percentiles), while the eastern half will likely experience increased extreme wet conditions (95th percentile). January projects rainfall increases in the eastern interior, with extreme wet conditions increasing by 35–45 mm across scenarios. Conversely, October may experience increased extreme dry conditions (5th percentile), with more than 48 mm decrease in the far-future under SSP5-8.5. During austral summer (DJF), pronounced wet and dry extremes are projected over eastern South Africa. Austral winter (JJA) will likely experience persistent and intensifying dry and wet extremes along the coast, with the southwest Cape particularly vulnerable to severe dry conditions. Heavy rainfall days are projected to increase in eastern South Africa, exceeding 10 days in the eastern interior. This study is crucial for understanding rainfall extremes under a changing atmospheric circulation and unpins more effective climate change adaptation strategies in South Africa. [ABSTRACT FROM AUTHOR] – Name: AbstractSuppliedCopyright Label: Group: Ab Data: <i>Copyright of Climate Dynamics is the property of Springer Nature and its content may not be copied or emailed to multiple sites without the copyright holder's express written permission. Additionally, content may not be used with any artificial intelligence tools or machine learning technologies. However, users may print, download, or email articles for individual use. This abstract may be abridged. No warranty is given about the accuracy of the copy. Users should refer to the original published version of the material for the full abstract.</i> (Copyright applies to all Abstracts.) |
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| RecordInfo | BibRecord: BibEntity: Identifiers: – Type: doi Value: 10.1007/s00382-026-08079-2 Languages: – Code: eng Text: English PhysicalDescription: Pagination: PageCount: 29 StartPage: 1 Titles: – TitleFull: Projections of extreme rainfall in South Africa using CMIP6 ISIMIP models. Type: main BibRelationships: HasContributorRelationships: – PersonEntity: Name: NameFull: Mohomi, Tumelo – PersonEntity: Name: NameFull: Stepanenko, Victor – PersonEntity: Name: NameFull: Medvedev, Alexander – PersonEntity: Name: NameFull: Dhau, Inos – PersonEntity: Name: NameFull: Chikoore, Hector – PersonEntity: Name: NameFull: Bopape, Mary-Jane IsPartOfRelationships: – BibEntity: Dates: – D: 01 M: 03 Text: Mar2026 Type: published Y: 2026 Identifiers: – Type: issn-print Value: 09307575 Numbering: – Type: volume Value: 64 – Type: issue Value: 3 Titles: – TitleFull: Climate Dynamics Type: main |
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