J. E. Hay
This paper reviews the theoretical basis of relatively simple models that use widely available meteorological data to determine the solar irradiation at the earth's surface. Spectral and non-spectral models for clear and cludy sky conditions are considered. A sample of validation results is presented. These indicate that most of the models studied are capable of estimating the global irradiation with acceptable accuracy, especially for time intervals of a month of more.
© 2001-2024 Fundación Dialnet · Todos los derechos reservados