Cloudiness Information Services for Solar Energy Management in West Africa
In West Africa (WA), interest in solar energy development has risen in recent years with many planned and ongoing projects currently in the region. However, a major drawback to this development in the region is the intense cloud cover that reduces the incoming solar radiation when present and causes...
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| Format: | Article |
| Language: | English |
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MDPI AG
2020-08-01
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| Series: | Atmosphere |
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| Online Access: | https://www.mdpi.com/2073-4433/11/8/857 |
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| author | Derrick Kwadwo Danso Sandrine Anquetin Arona Diedhiou Rabani Adamou |
| author_facet | Derrick Kwadwo Danso Sandrine Anquetin Arona Diedhiou Rabani Adamou |
| author_sort | Derrick Kwadwo Danso |
| collection | DOAJ |
| description | In West Africa (WA), interest in solar energy development has risen in recent years with many planned and ongoing projects currently in the region. However, a major drawback to this development in the region is the intense cloud cover that reduces the incoming solar radiation when present and causes fluctuations in solar power production. Therefore, understanding the occurrence of clouds and their link to the surface solar radiation in the region is important for making plans to manage future solar energy production. In this study, we use the state-of-the-art European Centre for Medium-range Weather Forecasts ReAnalysis (ERA5) dataset to examine the occurrence and persistence of cloudy and clear-sky conditions in the region. Then, we investigate the effects of cloud cover on the quantity and variability of the incoming solar radiation. The cloud shortwave radiation attenuation (<inline-formula><math display="inline"><semantics><mrow><mi>C</mi><mi>R</mi><msubsup><mi>A</mi><mrow><mi>S</mi><mi>W</mi></mrow><mo>↓</mo></msubsup></mrow></semantics></math></inline-formula>) is used to quantify the amount of incoming solar radiation that is lost due to clouds. The results showed that the attenuation of incoming solar radiation is stronger in all months over the southern part of WA near the Guinea Coast. Across the whole region, the maximum attenuation occurs in August, with a mean <inline-formula><math display="inline"><semantics><mrow><mi>C</mi><mi>R</mi><msubsup><mi>A</mi><mrow><mi>S</mi><mi>W</mi></mrow><mo>↓</mo></msubsup></mrow></semantics></math></inline-formula> of about 55% over southern WA and between 20% and 35% in the Sahelian region. Southern WA is characterized by a higher occurrence of persistent cloudy conditions, while the Sahel region and northern WA are associated with frequent clear-sky conditions. Nonetheless, continuous periods with extremely low surface solar radiation were found to be few over the whole region. The analysis also showed that the surface solar radiation received from November to April only varies marginally from one year to the other. However, there is a higher uncertainty during the core of the monsoon season (June to October) with regard to the quantity of incoming solar radiation. The results obtained show the need for robust management plans to ensure the long-term success of solar energy projects in the region. |
| first_indexed | 2024-03-10T17:30:07Z |
| format | Article |
| id | doaj.art-e05e3816e60e47baaaf240dac386bdde |
| institution | Directory Open Access Journal |
| issn | 2073-4433 |
| language | English |
| last_indexed | 2024-03-10T17:30:07Z |
| publishDate | 2020-08-01 |
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| series | Atmosphere |
| spelling | doaj.art-e05e3816e60e47baaaf240dac386bdde2023-11-20T10:04:25ZengMDPI AGAtmosphere2073-44332020-08-0111885710.3390/atmos11080857Cloudiness Information Services for Solar Energy Management in West AfricaDerrick Kwadwo Danso0Sandrine Anquetin1Arona Diedhiou2Rabani Adamou3Université Grenoble Alpes, IRD, CNRS, Grenoble-INP, IGE, 38000 Grenoble, FranceUniversité Grenoble Alpes, IRD, CNRS, Grenoble-INP, IGE, 38000 Grenoble, FranceUniversité Grenoble Alpes, IRD, CNRS, Grenoble-INP, IGE, 38000 Grenoble, FranceWASCAL GRP on Climate Change and Energy, Faculté des Sciences et Techniques, Université Abdou Moumouni, Niamey , NigerIn West Africa (WA), interest in solar energy development has risen in recent years with many planned and ongoing projects currently in the region. However, a major drawback to this development in the region is the intense cloud cover that reduces the incoming solar radiation when present and causes fluctuations in solar power production. Therefore, understanding the occurrence of clouds and their link to the surface solar radiation in the region is important for making plans to manage future solar energy production. In this study, we use the state-of-the-art European Centre for Medium-range Weather Forecasts ReAnalysis (ERA5) dataset to examine the occurrence and persistence of cloudy and clear-sky conditions in the region. Then, we investigate the effects of cloud cover on the quantity and variability of the incoming solar radiation. The cloud shortwave radiation attenuation (<inline-formula><math display="inline"><semantics><mrow><mi>C</mi><mi>R</mi><msubsup><mi>A</mi><mrow><mi>S</mi><mi>W</mi></mrow><mo>↓</mo></msubsup></mrow></semantics></math></inline-formula>) is used to quantify the amount of incoming solar radiation that is lost due to clouds. The results showed that the attenuation of incoming solar radiation is stronger in all months over the southern part of WA near the Guinea Coast. Across the whole region, the maximum attenuation occurs in August, with a mean <inline-formula><math display="inline"><semantics><mrow><mi>C</mi><mi>R</mi><msubsup><mi>A</mi><mrow><mi>S</mi><mi>W</mi></mrow><mo>↓</mo></msubsup></mrow></semantics></math></inline-formula> of about 55% over southern WA and between 20% and 35% in the Sahelian region. Southern WA is characterized by a higher occurrence of persistent cloudy conditions, while the Sahel region and northern WA are associated with frequent clear-sky conditions. Nonetheless, continuous periods with extremely low surface solar radiation were found to be few over the whole region. The analysis also showed that the surface solar radiation received from November to April only varies marginally from one year to the other. However, there is a higher uncertainty during the core of the monsoon season (June to October) with regard to the quantity of incoming solar radiation. The results obtained show the need for robust management plans to ensure the long-term success of solar energy projects in the region.https://www.mdpi.com/2073-4433/11/8/857cloud coversolar energysurface solar radiationattenuationWest AfricaERA5 |
| spellingShingle | Derrick Kwadwo Danso Sandrine Anquetin Arona Diedhiou Rabani Adamou Cloudiness Information Services for Solar Energy Management in West Africa Atmosphere cloud cover solar energy surface solar radiation attenuation West Africa ERA5 |
| title | Cloudiness Information Services for Solar Energy Management in West Africa |
| title_full | Cloudiness Information Services for Solar Energy Management in West Africa |
| title_fullStr | Cloudiness Information Services for Solar Energy Management in West Africa |
| title_full_unstemmed | Cloudiness Information Services for Solar Energy Management in West Africa |
| title_short | Cloudiness Information Services for Solar Energy Management in West Africa |
| title_sort | cloudiness information services for solar energy management in west africa |
| topic | cloud cover solar energy surface solar radiation attenuation West Africa ERA5 |
| url | https://www.mdpi.com/2073-4433/11/8/857 |
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