Anisotropic approach to calculate solar radiation on a tilted surface.
Hay and Davies (1980) estimate the fraction of the diffuse that is circumsolar and consider it to be all from the same direction as the beam radiation; they do not treat horizon brightening. Reindl et al. (1990b) add a horizon-brightening term to the Hay and Davies model, as proposed by Klucher (1979), giving a model to be
referred to as the HDKR model (see Duffie & Beckman, 2006).
Theoretical model based on the assumption that the diffuse irradiance has a peak next to the angle of the sun so that this circumsolar irradiance can be added to direct irradiance.
Usage for small values of angleOfSunIncidence.horizontal is not recommended because of refraction by atmosphere.
(no remarks)
direct_tilted, diffuse_tilted and ground_tilted are the calculated irradiances of tilted surface.
None.
Purely theoretical model
Duffie & Beckman (2006): Solar Engineering of Thermal Processes, p. 91 f.
Model created by Tobias Toerber (tobias.toerber@tuhh.de), Jul 2015
Edited by Sascha Guddusch (sascha.guddusch@tuhh.de), May 2016
Modified by Anne Senkel (anne.senkel@tuhh.de), Mar 2017
Modified by Lisa Andresen (andresen@tuhh.de), Apr. 2017
Model modified by Oliver Schülting (oliver.schuelting@tuhh.de), Jun 2018: no anisotropy if irradiance_extraterrestrial<=25 since this lead to unrealistic high irradiation peaks at morning and/or evening