This component computes the hemispherical diffuse irradiation
on a tilted surface using an isotropic model.
The irradiation is a sum composed of diffuse solar irradiation and
radiation reflected by the ground.
For a definition of the parameters, see the
User's Guide.
References
P. Ineichen, R. Perez and R. Seals (1987).
The Importance of Correct Albedo Determination for Adequately Modeling
Energy Received by Tilted Surface,
Solar Energy, 39(4): 301-305.
-
November 14, 2015, by Michael Wetter:
Added min
, max
and unit
attributes for rho
.
-
June 6, 2012, by Wangda Zuo:
Added contributions from sky and ground that were separated in base class.
-
May 24, 2010, by Wangda Zuo:
First implementation.
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