Simple approximation of the anisotropic diurnal heat (Ha) distribution
Usage
dahi(x, amax = 202.5)
Value
terra SpatRaster class object Diurnal Anisotropic Heat Index
Arguments
x
An elevation raster of class terra SpatRaster
amax
The Alpha Max (amax) parameter in degrees defined
as: minimum = 0, maximum = 360 with the default = 202.500
Author
Jeffrey S. Evans <jeffrey_evans@tnc.org>
Details
The Diurnal Anisotropic Heat Index is based on this equation.
Ha = cos(amax - a) * arctan(b)
Where; amax defines the aspect with the maximum total heat
surplus, a is the aspect and b is the slope angle.
References
Boehner, J., and Antonic, O. (2009) Land-surface parameters specific to
topo-climatology. In: Hengl, T., & Reuter, H. (Eds.), Geomorphometry -
Concepts, Software, Applications. Developments in Soil Science,
33:195-226