Simulating evapotranspiration in a semi-arid environment

H Hübener, M Schmidt, M Sogalla… - Theoretical and Applied …, 2005 - Springer
In this work, simulations with the mesoscale meteorological model FOOT3DK for a semi-arid
research site in southern morocco are presented. The main aim of this study is to introduce …

Calibration of an evapotranspiration model to simulate soil water dynamics in a semiarid rangeland

MP Maneta, S Schnabel, WW Wallender… - Hydrological …, 2008 - Wiley Online Library
Soil is the largest reservoir of water in a catchment and evapotranspiration is the largest
yearly output flux of water from the soil in semiarid environments at the catchment scale …

Daily potential evapotranspiration and diurnal climate forcings: influence on the numerical modelling of soil water dynamics and evapotranspiration

S Liu, WD Graham, JM Jacobs - Journal of Hydrology, 2005 - Elsevier
A physically based, variably saturated flow model was developed to predict soil water
dynamics, evapotranspiration (ET) from the vadose zone, and recharge to (or exfiltration …

Simulation of soil moisture and evapotranspiration in a soil profile during the 1999 MAP-Riviera Campaign

M Zappa, J Gurtz - Hydrology and Earth System Sciences, 2003 - hess.copernicus.org
Detailed plot-scale observations of basic hydrometeorological variables represent valuable
data for assessing the quality of the soil moisture module and evapotranspiration scheme in …

A parameterization of evaporation from bare soil surfaces

J Kondo, N Saigusa, T Sato - Journal of Applied Meteorology …, 1990 - journals.ametsoc.org
A simple model of evaporation from a bare soil surface is developed. This model combines
two processes of water vapor transport: one is the vapor transport in air expressed by the …

A numerical approach to calculating soil wetness and evapotranspiration over large grid areas

PJ Sellers, MJ Fennessy… - Journal of Geophysical …, 2007 - Wiley Online Library
Soil wetness is typically highly variable in space over the length scales of general circulation
model grid areas (∼ 100 km), and the stress functions relating the surface …

Study of the mechanisms of evaporation under arid conditions using a detailed model of the soil–atmosphere continuum. Application to the EFEDA I experiment

G Boulet, I Braud, M Vauclin - Journal of Hydrology, 1997 - Elsevier
As part of the framework of the EFEDA (Echieval field experiment in a desertification
threatened area) experiment, an 11-day data set including atmospheric forcing, turbulent …

Modeling Land–Atmosphere Interactions over Semiarid Plains in Morocco: In-Depth Assessment of GCM Stretched-Grid Simulations Using In Situ Data

K Arjdal, É Vignon, F Driouech… - Journal of Applied …, 2024 - journals.ametsoc.org
Land surface–atmosphere interactions are a key component of climate modeling. They are
particularly critical to understand and anticipate the climate and the water resources over the …

[HTML][HTML] A comparison of continuous soil moisture simulations using different soil hydraulic parameterizations for a site in Germany

G Schädler - Journal of applied meteorology and climatology, 2007 - journals.ametsoc.org
Continuous time series of soil water content over a period of more than 9 months for a
midlatitude sandy loam soil covered by grass are calculated with the Campbell and the van …

A semiempirical model of bare soil evaporation for crop simulation models

N Brisson, A Perrier - Water resources research, 1991 - Wiley Online Library
In crop simulation models the water subroutine computes evaporation and transpiration
separately. This property allows a greater confidence in the simulation of the early crop …