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i.evapo.pt(1grass)          GRASS GIS User's Manual         i.evapo.pt(1grass)

NAME
       i.evapo.pt   -  Computes  evapotranspiration  calculation Priestley and
       Taylor formulation, 1972.

KEYWORDS
       imagery, evapotranspiration

SYNOPSIS
       i.evapo.pt
       i.evapo.pt --help
       i.evapo.pt  [-z]  net_radiation=name  soil_heatflux=name   air_tempera-
       ture=name  atmospheric_pressure=name  priestley_taylor_coeff=float out-
       put=name  [--overwrite]  [--help]  [--verbose]  [--quiet]  [--ui]

   Flags:
       -z
           Set negative ETa to zero

       --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:
       net_radiation=name [required]
           Name of input net radiation raster map [W/m2]

       soil_heatflux=name [required]
           Name of input soil heat flux raster map [W/m2]

       air_temperature=name [required]
           Name of input air temperature raster map [K]

       atmospheric_pressure=name [required]
           Name of input atmospheric pressure raster map [millibars]

       priestley_taylor_coeff=float [required]
           Priestley-Taylor coefficient
           Default: 1.26

       output=name [required]
           Name of output evapotranspiration raster map [mm/d]

DESCRIPTION
       i.evapo.pt Calculates the diurnal evapotranspiration after Prestley and
       Taylor  (1972). The Priestley-Taylor model (Priestley and Taylor, 1972)
       is a modification of Penman’s more theoretical equation.

NOTES
       RNETD optional output from i.evapo.potrad is giving good results as in-
       put for net radiation in this module.

       Alpha values:

           •   1.32  for estimates from vegetated areas as a result of the in-
               crease  in  surface  roughness  (Morton,  1983;  Brutsaert  and
               Stricker, 1979)

           •   1.26  is  applicable  in  humid climates (De Bruin and Keijman,
               1979; Stewart and Rouse, 1976; Shuttleworth and Calder,  1979),
               and temperate hardwood swamps (Munro, 1979)

           •   1.74  has  been recommended for estimating potential evapotran-
               spiration in more arid regions (ASCE, 1990). This  worked  well
               in Greece with University of Thessaloniki.
       Alpha values extracted from: Watflood manual.

SEE ALSO
        i.evapo.mh, i.evapo.pm, i.evapo.time, i.eb.netrad, r.sun

AUTHORS
       Yann Chemin, GRASS Development Team, 2007-08

SOURCE CODE
       Available at: i.evapo.pt source code (history)

       Accessed: unknown

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       © 2003-2022 GRASS Development Team, GRASS GIS 7.8.7 Reference Manual

GRASS 7.8.7                                                 i.evapo.pt(1grass)

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