Yacouba Yira, T. C. Mutsindikwa, A. Bossa, Jean Hounkpè, S. Salack
{"title":"评估气候变化对Bamboi流域水电潜力的影响(西非Black Volta)","authors":"Yacouba Yira, T. C. Mutsindikwa, A. Bossa, Jean Hounkpè, S. Salack","doi":"10.5194/piahs-384-349-2021","DOIUrl":null,"url":null,"abstract":"Abstract. This study evaluates the impact of future climate change (CC) on\nthe hydropower generation potential of the Bamboi catchment (Black Volta) in\nWest Africa using a conceptual rainfall-runoff model (HBV light) and\nregional climate models (RCMs)–global climate models (GCMs). Two climate\nsimulation datasets MPI-ESM-REMO (CORDEX) and GFDL-ESM2M-WRF (WASCAL) under\nRCP4.5 were applied to the validated hydrological model to simulate the\ncatchment runoff. Based on reference and future simulated discharges, a\ntheoretical 1.3 MW run of river hydro power plant was designed to evaluate\nthe hydropower generation. Hydrological and hydropower generation changes\nwere expressed as the relative difference between two future periods\n(2020–2049 and 2070–2099) and a reference period (1983–2005). The climate\nmodels' ensemble projected a mean annual precipitation increase by 8.8 %\nand 7.3 % and discharge increase by 11.4 % and 9.735 % for the\n2020–2049 and 2070–2099 periods respectively (for bias corrected data). On\nthe contrary an overall decrease of hydropower generation by −9.1 % and\n−8.4% for the 2020–2049 and 2070–2099 periods was projected\nrespectively. The results indicate that projected increases in discharge\nshould not solely be considered as leading to an increase in hydropower\npotential when prospecting climate change impact on hydropower.\n","PeriodicalId":53381,"journal":{"name":"Proceedings of the International Association of Hydrological Sciences","volume":null,"pages":null},"PeriodicalIF":0.0000,"publicationDate":"2021-11-16","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"1","resultStr":"{\"title\":\"Assessing climate change impact on the hydropower potential of the Bamboi catchment (Black Volta, West Africa)\",\"authors\":\"Yacouba Yira, T. C. Mutsindikwa, A. Bossa, Jean Hounkpè, S. Salack\",\"doi\":\"10.5194/piahs-384-349-2021\",\"DOIUrl\":null,\"url\":null,\"abstract\":\"Abstract. This study evaluates the impact of future climate change (CC) on\\nthe hydropower generation potential of the Bamboi catchment (Black Volta) in\\nWest Africa using a conceptual rainfall-runoff model (HBV light) and\\nregional climate models (RCMs)–global climate models (GCMs). Two climate\\nsimulation datasets MPI-ESM-REMO (CORDEX) and GFDL-ESM2M-WRF (WASCAL) under\\nRCP4.5 were applied to the validated hydrological model to simulate the\\ncatchment runoff. Based on reference and future simulated discharges, a\\ntheoretical 1.3 MW run of river hydro power plant was designed to evaluate\\nthe hydropower generation. Hydrological and hydropower generation changes\\nwere expressed as the relative difference between two future periods\\n(2020–2049 and 2070–2099) and a reference period (1983–2005). The climate\\nmodels' ensemble projected a mean annual precipitation increase by 8.8 %\\nand 7.3 % and discharge increase by 11.4 % and 9.735 % for the\\n2020–2049 and 2070–2099 periods respectively (for bias corrected data). On\\nthe contrary an overall decrease of hydropower generation by −9.1 % and\\n−8.4% for the 2020–2049 and 2070–2099 periods was projected\\nrespectively. The results indicate that projected increases in discharge\\nshould not solely be considered as leading to an increase in hydropower\\npotential when prospecting climate change impact on hydropower.\\n\",\"PeriodicalId\":53381,\"journal\":{\"name\":\"Proceedings of the International Association of Hydrological Sciences\",\"volume\":null,\"pages\":null},\"PeriodicalIF\":0.0000,\"publicationDate\":\"2021-11-16\",\"publicationTypes\":\"Journal Article\",\"fieldsOfStudy\":null,\"isOpenAccess\":false,\"openAccessPdf\":\"\",\"citationCount\":\"1\",\"resultStr\":null,\"platform\":\"Semanticscholar\",\"paperid\":null,\"PeriodicalName\":\"Proceedings of the International Association of Hydrological Sciences\",\"FirstCategoryId\":\"1085\",\"ListUrlMain\":\"https://doi.org/10.5194/piahs-384-349-2021\",\"RegionNum\":0,\"RegionCategory\":null,\"ArticlePicture\":[],\"TitleCN\":null,\"AbstractTextCN\":null,\"PMCID\":null,\"EPubDate\":\"\",\"PubModel\":\"\",\"JCR\":\"Q3\",\"JCRName\":\"Earth and Planetary Sciences\",\"Score\":null,\"Total\":0}","platform":"Semanticscholar","paperid":null,"PeriodicalName":"Proceedings of the International Association of Hydrological Sciences","FirstCategoryId":"1085","ListUrlMain":"https://doi.org/10.5194/piahs-384-349-2021","RegionNum":0,"RegionCategory":null,"ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"Q3","JCRName":"Earth and Planetary Sciences","Score":null,"Total":0}
Assessing climate change impact on the hydropower potential of the Bamboi catchment (Black Volta, West Africa)
Abstract. This study evaluates the impact of future climate change (CC) on
the hydropower generation potential of the Bamboi catchment (Black Volta) in
West Africa using a conceptual rainfall-runoff model (HBV light) and
regional climate models (RCMs)–global climate models (GCMs). Two climate
simulation datasets MPI-ESM-REMO (CORDEX) and GFDL-ESM2M-WRF (WASCAL) under
RCP4.5 were applied to the validated hydrological model to simulate the
catchment runoff. Based on reference and future simulated discharges, a
theoretical 1.3 MW run of river hydro power plant was designed to evaluate
the hydropower generation. Hydrological and hydropower generation changes
were expressed as the relative difference between two future periods
(2020–2049 and 2070–2099) and a reference period (1983–2005). The climate
models' ensemble projected a mean annual precipitation increase by 8.8 %
and 7.3 % and discharge increase by 11.4 % and 9.735 % for the
2020–2049 and 2070–2099 periods respectively (for bias corrected data). On
the contrary an overall decrease of hydropower generation by −9.1 % and
−8.4% for the 2020–2049 and 2070–2099 periods was projected
respectively. The results indicate that projected increases in discharge
should not solely be considered as leading to an increase in hydropower
potential when prospecting climate change impact on hydropower.