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NAME

i.eb.eta - actual evapotranspiration for diurnal period (Bastiaanssen, 1995)

KEYWORDS

imagery, actual evapotranspiration, energy balance, SEBAL

SYNOPSIS

i.eb.eta
i.eb.eta help
i.eb.eta netradiationdiurnal=name evaporativefraction=name temperature=name output=name [--overwrite] [--verbose] [--quiet]

Flags:

--overwrite
Allow output files to overwrite existing files
--verbose
Verbose module output
--quiet
Quiet module output

Parameters:

netradiationdiurnal=name
Name of the diurnal Net Radiation map [W/m2]
Default: rnetday
evaporativefraction=name
Name of the evaporative fraction map [-]
Default: evapfr
temperature=name
Name of the surface skin temperature [K]
Default: tempk
output=name
Name of the output actual evapotranspiration layer [mm/d]

DESCRIPTION

i.eb.eta calculates the actual evapotranspiration (ETa ; mm/d) for diurnal period after [1], implemented in [3]. It takes input of Diurnal Net Radiation (see r.sun), evaporative fraction (see r.eb.evapfr) and surface skin temperature.

NOTES

Full ETa processing will need those: (for time integration: i.evapo.time_integration)

For more details on the algorithms see [1][2][3].

TODO

SEE ALSO

r.sun
i.eb.evapfr
i.eb.netrad

REFERENCES

[1] Bastiaanssen, W.G.M., 1995. Estimation of Land surface paramters by remote sensing under clear-sky conditions. PhD thesis, Wageningen University, Wageningen, The Netherlands.

[2] Chemin Y., Alexandridis T.A., 2001. Improving spatial resolution of ET seasonal for irrigated rice in Zhanghe, China. Asian Journal of Geoinformatics. 5(1):3-11,2004.

[3] Alexandridis T.K., Cherif I., Chemin Y., Silleos N.G., Stavrinos E., Zalidis G.C. Integrated methodology for estimating water use in Mediterranean agricultural areas. Remote Sensing. -(-):,2009. (submitted))

AUTHORS

Yann Chemin, Asian Institute of Technology, Thailand

Last changed: $Date: 2009-06-19 14:16:20 -0700 (Fri, 19 Jun 2009) $


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