Variation of Solar Radiation in Akwanga, Nasarawa State, Nigeria

dc.contributor.authorMamman, Adah
dc.contributor.authorIbrahim, Umar
dc.contributor.authorDauda, Samson Yusuf
dc.contributor.authorMustapha, Mohammed Yusuf
dc.contributor.authorPaul, Bartholomew
dc.date.accessioned2023-12-14T07:51:58Z
dc.date.available2023-12-14T07:51:58Z
dc.date.issued2020-06-05
dc.description.abstractOne of the major environmental problem is the long-term changes in the Earth’s climate. In this study, the variation of solar radiation for Akwanga zone, Nasarawa State, Nigeria were determined. Twelve locations were carefully selected where there is no sunshine and wind obstruction. Three 12V, 5W Solar panels (poly) were used and a three-hour daily measurement interval (12.00 pm to 3.00 pm) was made using the Secondary Standard Pyranometer placed on the top of the panels. Angstrom-Prescott Regression Equation was used to estimate the output. The continuity in the assembled system was measured using an Avometer. The result revealed that the highest monthly average daily global solar radiation was observed in the month of April (25.2 MJ/m2) followed by June (22.94 MJ/m2), and march (22.42 MJ/m2), while the lowest was observed in the month of August (12.04 MJ/m2) followed by July (13.57 MJ/m2), and September (14.26 MJ/m2) in the locations selected. The solar radiation intensity was found to range from 156.44 W/m2 to 293.84 W/m2 with the mean value of 220.04 W/m2. The highest total global solar radiation value of 25.2MJ/m2 was observed in April while the lowest value of 12.04 MJ/m2 was observed in October. The extraterrestrial solar radiation were found to range from 16.72 MJ/m2 in March to 29.90 MJ/m2 in April with average value of 22.89MJ/m2. The atmospheric transmission coefficient over the year is found to range from 0.5 in July and October to 1.3 in June and October. The investigation reveal that there is bright sun shine in the study area which confirms high atmospheric transmission coefficient or clearness index throughout the year in this study.en_US
dc.identifier.citation1. Wald L. Solar radiation energy (fundamentals); Solar energy conversion Radiation Energy (Fundamentals); 2007. 2. Pandey CK, Katiyar AK. Solar radiation: Models and measurement techniques. J. Energy. 2013;305207. 3. Adekunle AO, Emmanuel CO, Stephen BO, Olugbenga F. Analysis of global solar irradiance over climatic zones in Nigeria for solar energy applications. Journal of Solar Energy. 2015;5(1):1-9. DOI:http://dx.doi.org/10.1155/2015/819307 4. Adesina MA, Ibrahim JS, Iortyer HA. A simulation model for estimating solar radiation of Nasarawa, Nasarawa State – Nigeria. British Journal of Applied Science & Technology. 2016;17(2):1-8. Article no.BJAST.24603. ISSN: 2231-0843, NLM ID: 101664541. 5. Donatelli M, Bellocchi G, Fontana F. RadEst3.00: Software to estimate daily radiation data from commonly available meteorological variables. European Journal of Agronomy. 2003;18(3-4):363– 367en_US
dc.identifier.urihttps://keffi.nsuk.edu.ng/handle/20.500.14448/6047
dc.language.isoenen_US
dc.publisherDepartment of Physics, Nasarawa State University Keffien_US
dc.subjectSolar radiation; pyranometer; Akwanga zone; daily global radiation.en_US
dc.titleVariation of Solar Radiation in Akwanga, Nasarawa State, Nigeriaen_US
dc.typeArticleen_US

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