Comparison of solar radiation calculation methods

This table compares two solar flux calculation methods in thermal simulations: one based on atmospheric extinction coefficients, and another based on altitude and turbidity.

Attribute Using atmospheric extinction coefficient Using altitude and turbidity
Model basis Empirical formula using extinction coefficient and the solar altitude angle Physics-based model using altitude, Linke turbidity, and Rayleigh scattering
Atmospheric effects Adjustment using empirical clearness factor Detailed turbidity modeling using Linke factor and Rayleigh optical thickness
Altitude correction Not included Included via air pressure adjustment and modified air mass
Use cases
  • When atmospheric clarity and solar position vary significantly over time or location.
  • When shadowing effects are either negligible or can be approximated separately.
  • For high-altitude locations, areas with variable atmospheric clarity (turbidity), or under cloudy conditions.
  • When shadowing effects are significant.