Determining the Level of Global Solar Radiation on the Earth's Surface
Zdenek Dostal, Miroslav Dulik
DOI: 10.15598/aeee.v13i5.1391
Abstract
The article analyzes the Earth's surface insolation. For the analysis, two methods are described - the method of approximate calculation and turbidity method using Linke turbidity index. The methods consider the latitude of current location on the Earth's surface, atmosphere attenuation and other major factors. To obtain more accurate values, long-term measurements at the current location should be obtained.