This is the command i.eb.netradgrass that can be run in the OnWorks free hosting provider using one of our multiple free online workstations such as Ubuntu Online, Fedora Online, Windows online emulator or MAC OS online emulator
PROGRAM:
NAME
i.eb.netrad - Net radiation approximation (Bastiaanssen, 1995).
KEYWORDS
imagery, energy balance, net radiation, SEBAL
SYNOPSIS
i.eb.netrad
i.eb.netrad --help
i.eb.netrad albedo=name ndvi=name temperature=name localutctime=name
temperaturedifference2m=name emissivity=name transmissivity_singleway=name dayofyear=name
sunzenithangle=name output=name [--overwrite] [--help] [--verbose] [--quiet] [--ui]
Flags:
--overwrite
Allow output files to overwrite existing files
--help
Print usage summary
--verbose
Verbose module output
--quiet
Quiet module output
--ui
Force launching GUI dialog
Parameters:
albedo=name [required]
Name of albedo raster map [0.0;1.0]
ndvi=name [required]
Name of NDVI raster map [-1.0;+1.0]
temperature=name [required]
Name of surface temperature raster map [K]
localutctime=name [required]
Name of time of satellite overpass raster map [local time in UTC]
temperaturedifference2m=name [required]
Name of the difference map of temperature from surface skin to about 2 m height [K]
emissivity=name [required]
Name of the emissivity map [-]
transmissivity_singleway=name [required]
Name of the single-way atmospheric transmissivitymap [-]
dayofyear=name [required]
Name of the Day Of Year (DOY) map [-]
sunzenithangle=name [required]
Name of the sun zenith angle map [degrees]
output=name [required]
Name of the output net radiation layer
DESCRIPTION
i.eb.netrad calculates the net radiation at the time of satellite overpass, the way it is
in the SEBAL model of Bastiaanssen (1995). It takes input of Albedo, NDVI, Surface Skin
temperature, time of satellite overpass, surface emissivity, difference of temperature
from surface skin and about 2 m height (dT), instantaneous satellite overpass single-way
atmospheric transmissivity (tsw), Day of Year (DOY), and sun zenith angle.
NOTES
In the old methods, dT was taken as flat images (dT=5.0), if you don’t have a dT map from
ground data, you would want to try something in this line, this is to calculate
atmospherical energy balance. In the same way, a standard tsw is used in those equations.
Refer to r_net.c for that and for other non-used equations, but stored in there for
further research convenience.
TODO
Add more explanations.
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