&r diffusb <dem> <out> <lat> <dstart> <dend> <timeint>
where: trn = the DEM grid; out
= is the radiation output grid; dem = file name of DEM; out
= base name of outgrid file names; lat = latitude
of study site (DEM) in decimal degrees; dstart = the start day (in
Julian day); dend = the time interval in minutes to calculate sun
positions (used for interpolating the energy budget; timeint = the
time interval in minutes to calculate sun positions (used for interpolating
the energy budget.
If dend is set equal to dstart then a single day is calculated with this routine. .
All the other requirements are the same as for running the shortwavc.aml
This is a complementary calculation to the direct radiation modeling. The
portion of diffuse solar radiation relative to the global radiation varies
between summer and winter, and is a function of solar altitude and terrain
reflectance, among other. Global radiation (the sum of direct and diffuse
radiation) is often used in other biophysical modeling application (e.g.
modeling of potential evapotranspiration, 3.1 – 3.3).
| Command: | &r diffuseb |
| Required input: | DEM |
| Output units: | kJ/m2/time period |
| Speed of calculations: | Very fast due to parsimonious programming |
| Flexibility of the routine: | Medium; can’t go beyond 1 day |
| User interface: | Limited, but simple and easy |
| Known errors: | - |
| Corrections | 9/14/2000: Adjustments to bug in ArcInfo 8.0.2 |
| Programmer | L. Kumar (original coding)
N.E. Zimmermann (code adjustments) |
| Download: | diffuseb.aml (use: "save link as") |
| Contact: | niklaus.zimmermann @ wsl.ch |
References:
Kumar, L., Skidmore, A.K. and Knowles, E., 1997. Modelling topographic variation in solar radiation in a GIS environment. International Journal for Geographical Information Science, 11(5): 475-497.Last Updated: 9/24/03