Abstract
In hydrological modeling, a correct description of the energy and mass exchanges at the interface between land and atmosphere is of primary importance. This is due to the fact that if the watershed boundary is correctly determined, the only water supply is rainfall, and evapotranspiration involves more than the half of the total amount of precipitation in temperate regions.
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References
Boatwright GO, Whitehead VS (1986) Early warning and crop condition assessment research. IEEE Trans Geos Remote Sens GE-24(1):54–64.
Deardorff JW (1977) A parametrization of ground surface moisture content for use in atmospheric prediction models. J Appl Meteorol 16:1182–1185.
Deardorff JW (1978) Efficient prediction of ground surface temperature and moisture, with inclusion of a layer of vegetation. J Geophys Res 83(4): 1889–1903.
Girard G (1974) Modelè global ORSTOM. Première application du modèle journalier à discretisation spatiale sur le bassin versant de la crique Grégoire en Guyane in “Atelier hydrologique sur les modèles mathématiques”. ORSTOM, Paris.
Jackson RD, Reginato RJ, Idso SB (1977) Wheat canopy temperature: A practical tool for evaluating water requirements. Water Resour Res 13:651–656.
Jackson RD, Idso SB, Reginato RJ, Pinter PJ Jr (1981) Canopy temperature as a crop water stress indicator. Water Resour Res 17(4): 1133–1138.
Ledoux E (1980) Modélisation intégrée des écoulements de surface et des écoulements souterrains sur un bassin hydrologique. Thèse de Docteur-Ingénieur, Ecole Nat. Supérieure des Mines de Paris et Université P et M Curie, Paris.
Manabé S (1969) The atmospheric circulation and the hydrology of the Earth’s surface. Mon Weather Rev 97:739–774.
Ottlé C, Vidal-Madjar D, Girard G (1989) Remote sensing applications to hydrological modeling. J Hydrol 105:369–384.
Soarès JV, Bernard R, Taconet O, Vidal-Madjar D, Weill A (1988) Estimation of a bare soil evaporation from airborne measurements. J Hydrol 99:281–296.
Taconet O, Bernard R, Vidal-Madjar D (1986) Evaporation over an agricultural region using a surface flux/temperature model based on NOAA/AVHRR data. J Clim Appl Meteorol 25:284–307.
Taconet O, Vidal-Madjar D (1988) Application of fluxes algorithm to a field campaign over a vegetated area. Remote Sens Environ 26(3): 227–239.
Therry G, Lacarrere P (1983) Improving the eddy kinetic energy model for planetary boundary layer description. Bound Layer Meteorol 25:63–88.
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© 1991 Springer-Verlag New York Inc.
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Ottlé, C., Vidal-Madjar, D. (1991). Introduction of a Realistic Soil-Vegetation Component in a Hydrological Model: Application to HAPEX-MOBILHY Experiment. In: Schmugge, T.J., André, JC. (eds) Land Surface Evaporation. Springer, New York, NY. https://doi.org/10.1007/978-1-4612-3032-8_7
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DOI: https://doi.org/10.1007/978-1-4612-3032-8_7
Publisher Name: Springer, New York, NY
Print ISBN: 978-0-387-97359-3
Online ISBN: 978-1-4612-3032-8
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