2018
DOI: 10.1007/s40095-018-0279-3
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A novel time-effective model for daily distributed solar radiation estimates across variable terrain

Abstract: Accurate and precisess estimation of spatio-temporal variability of solar radiation is critical. Some commonly used models evaluate this variability using methods in which the data required for estimating atmospheric attenuation may not be easily accessible for some study areas. Here, a daily solar radiation estimation method which uses ambient air temperature, a Digital Elevation Model, time of year, and monthly radiation estimates from Solar Analyst model has been proposed. The objective was to use air tempe… Show more

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Cited by 9 publications
(5 citation statements)
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“…Cloud cover has the largest influence on radiation attenuation in the atmosphere [27]. Solar analyst uses defined default values for the diffuse proportion of global radiation (k D ) and the ratio of the insolation received at the Earth's surface as direct radiation along the shortest atmospheric path at sea level to the insolation at the upper border of the atmosphere ( sl , transmittivity), which should be adjusted for local atmospheric conditions [11,20,45]. Accordingly, utilizing meteorological measured [8] data over 5 years from a station (Lethbridge CDA, located at 49°42′0″N, 112°46′60″W) inside the study region and calculating the actual values of required inputs (k D = 0.429, sl = 0.589 ), the effects of cloud cover and local atmospheric conditions have been included.…”
Section: Solar Resource Evaluationmentioning
confidence: 99%
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“…Cloud cover has the largest influence on radiation attenuation in the atmosphere [27]. Solar analyst uses defined default values for the diffuse proportion of global radiation (k D ) and the ratio of the insolation received at the Earth's surface as direct radiation along the shortest atmospheric path at sea level to the insolation at the upper border of the atmosphere ( sl , transmittivity), which should be adjusted for local atmospheric conditions [11,20,45]. Accordingly, utilizing meteorological measured [8] data over 5 years from a station (Lethbridge CDA, located at 49°42′0″N, 112°46′60″W) inside the study region and calculating the actual values of required inputs (k D = 0.429, sl = 0.589 ), the effects of cloud cover and local atmospheric conditions have been included.…”
Section: Solar Resource Evaluationmentioning
confidence: 99%
“…All meteorological data were obtained from Alberta Agriculture and Forestry, Alberta Climate Information Service (ACIS) (https ://agric ultur e.alber ta.ca/acis, retrieved 2016). Instead of sl in global annual solar radiation calculation, we used k T sl (the ratio of measured global solar radiation on a horizontal surface against the extraterrestrial radiation at sea level) [11]. Between 11:30 and 12:30 h for each day of the years 2010-2014, the hourly k T was evaluated for the station [46].…”
Section: Solar Resource Evaluationmentioning
confidence: 99%
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“…ARIMA time series forecast model was developed in [12] to predict the temperature in Pakistan and it also develops a linear trend model to estimate electric power consumption. Digital Elevation Models were developed in [13] to predict the solar irradiation.…”
Section: Introductionmentioning
confidence: 99%
“…Two temperature-based empirical models 15,16 are commonly used for solar radiation prediction. [17][18][19] The diurnal temperature range is considered in Hargreaves and Samani model as an indicator of the R a ratio that arrives at the surface of the earth. An exponential function between the diurnal temperature range and solar radiation was provided in Bristow and Campbell model.…”
mentioning
confidence: 99%