radiometric.surface.temp {bigleaf} | R Documentation |
Radiometric Surface Temperature
Description
Radiometric surface temperature from longwave radiation measurements.
Usage
radiometric.surface.temp(
data,
LW_up = "LW_up",
LW_down = "LW_down",
emissivity,
constants = bigleaf.constants()
)
Arguments
data |
Data.frame or matrix containing all required input variables |
LW_up |
Longwave upward radiation (W m-2) |
LW_down |
Longwave downward radiation (W m-2) |
emissivity |
Emissivity of the surface (-) |
constants |
sigma - Stefan-Boltzmann constant (W m-2 K-4) |
Details
Radiometric surface temperature (Trad) is calculated as:
Trad = ((LW_up - (1 - \epsilon)*LW_down) / (\sigma \epsilon))^(1/4)
Value
a data.frame with the following columns:
Trad_K |
Radiometric surface temperature (K) |
Trad_degC |
Radiometric surface temperature (degC) |
References
Wang, W., Liang, S., Meyers, T. 2008: Validating MODIS land surface temperature products using long-term nighttime ground measurements. Remote Sensing of Environment 112, 623-635.
Examples
# determine radiometric surface temperature for the site DE-Tha in June 2014
# assuming an emissivity of 0.98.
# (Note that variable 'LW_down' was only included for the DE-Tha example dataset
# and not for the others due restrictions on file size)
Trad <- radiometric.surface.temp(DE_Tha_Jun_2014,emissivity=0.98)
summary(Trad)
[Package bigleaf version 0.8.2 Index]