Session 3 : Models for determining evapotranspiration
310
precision (0.8 and 0.9mmday
-1
). In the first place a single layer model can be used while in the
second one for obtain a similar precision a more complex two layer model must be applied.
BIBLIOGRAPHY
Bolle, H.J. and Langer, I. 1991. Echival Field Experiment in a Desertification-Threatened Area
(EFEDA). Field Experiment Plan. Meteorological Institute, Free University of Berlin, Germany.
Coll, C., Caselles, V., Sobrino, J.A. and Valor, E. 1994. On the atmospheric dependence on the splitwindow equation for land surface temperature. Int.J. Remote Sensing (15)150-122.
Hurtado, E., Caselles, V. and Artigao, M.M. 1994. Estimating maize evapotranspiration from NOAAAVHRR thermal data in the Albacete area, Spain. Int.J. Remote Sensing (15)2023-2037.
Hurtado, E., Caselles, V. and Artigao, M.M. 1994. Mapping actual evapotranspiration by combining
landsat TM and NOAA AVHRR images in the Barrax (Albacete) region, Spain. Societé française
de photogrammétrie et télédétection(137) 47-49.
Jackson, R.D., Reginato, R.J. and Idso, S.B. 1977. Wheat canopy temperature:a practical tool for
evaluating water requirements .Water Resour. Res. (13). 651-656.
Kustas, W.P. 1990. Estimates of evapotranspiration with a one and two dimensional model of heat
transfer over partial canopy cover. J. Appl. Meteorol. (49). 135-153.
Shuttleworth, J.and Wallace, J.S. 1985.Evaporation from sparse crops-an energy combination
theory.Q.J.R. Meteorol. Soc.(111) 839-855.
Shuttleworth, J.and Gurney, R. 1990. The theoretical relationship between foliage temperature and
canopy resistance in sparse crops.Q.J.R. Meteorol. Soc.(116) 497-519.
310
precision (0.8 and 0.9mmday
-1
). In the first place a single layer model can be used while in the
second one for obtain a similar precision a more complex two layer model must be applied.
BIBLIOGRAPHY
Bolle, H.J. and Langer, I. 1991. Echival Field Experiment in a Desertification-Threatened Area
(EFEDA). Field Experiment Plan. Meteorological Institute, Free University of Berlin, Germany.
Coll, C., Caselles, V., Sobrino, J.A. and Valor, E. 1994. On the atmospheric dependence on the splitwindow equation for land surface temperature. Int.J. Remote Sensing (15)150-122.
Hurtado, E., Caselles, V. and Artigao, M.M. 1994. Estimating maize evapotranspiration from NOAAAVHRR thermal data in the Albacete area, Spain. Int.J. Remote Sensing (15)2023-2037.
Hurtado, E., Caselles, V. and Artigao, M.M. 1994. Mapping actual evapotranspiration by combining
landsat TM and NOAA AVHRR images in the Barrax (Albacete) region, Spain. Societé française
de photogrammétrie et télédétection(137) 47-49.
Jackson, R.D., Reginato, R.J. and Idso, S.B. 1977. Wheat canopy temperature:a practical tool for
evaluating water requirements .Water Resour. Res. (13). 651-656.
Kustas, W.P. 1990. Estimates of evapotranspiration with a one and two dimensional model of heat
transfer over partial canopy cover. J. Appl. Meteorol. (49). 135-153.
Shuttleworth, J.and Wallace, J.S. 1985.Evaporation from sparse crops-an energy combination
theory.Q.J.R. Meteorol. Soc.(111) 839-855.
Shuttleworth, J.and Gurney, R. 1990. The theoretical relationship between foliage temperature and
canopy resistance in sparse crops.Q.J.R. Meteorol. Soc.(116) 497-519.