Solar radiation is the main energy source for mankind and an accurate data of solar radiation levels for a particular location is vital for the optimum operation of solar energy transducers such as photovoltaic cells and solar thermal collectors. In this work, we show that there is a linear relationship between recorded monthly average temperatures and solar radiation in Swaziland. The correlation can be utilized to develop two mathematical models for the estimation of solar radiation: one from the measured monthly average temperatures and the other based on the square-root of the difference between measured maximum and minimum monthly average temperatures. Both models fit the data well and can be applied to estimate solar radiation in other parts of the region Keywords: solar energy; solar radiation; climatic data; solar radiation estimation.
INTRODUCTIONAn accurate knowledge of solar radiation levels for a particular location is a prerequisite in the determination of the performance of various solar energy transducers such as photovoltaic cells and solar thermal collectors. Solar radiation data is also important in disciplines such as building designs and agricultural processes, e.g. evapo-transpiration of plants. However, weather stations will, at times, not have data on solar radiation because the instruments for radiation measurement, such as pyrometers and solarimeters, may not be available. As a result, mathematical models have been developed and calibrated to estimate solar radiation in different parts of the world such as in Brazil (Dos Santos, 2014), Iran (Saffaripour, 2013), India (Bajpai, 2009), Algeria/Spain (Chegaar,1998), China (Li, 2014a; 2014b), Bangladesh (Datta, 2013), Chile (Meza, 2000), USA (Allen, 1997) and Nigeria (Umoh, 2013). These models estimate solar radiation as a function of meteorological parameters such as temperature, atmospheric pressure, relative humidity, the number of sunshine hours, wind speed, cloud cover, and rainfall.