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The hydrologic cycle is a system far from thermodynamic equilibrium that is characterized by its rate of entropy production in the climatological mean steady state. Over land, the hydrologic cycle is ...
Interactions between shallow groundwater and land surface processes play an important role in the ecohydrology of riparian zones. Some recent land surface models (LSMs) incorporate groundwater-land su...
We present an evapotranspiration (ET) model developed in the framework of the EUMETSAT "Satellite Application Facility" (SAF) on Land Surface Analysis (LSA). The model is a simplified Soil-Vegetation-...
Distributed energy and water balance models require time-series surfaces of the climatological variables involved in hydrological processes. Among them, solar radiation constitutes a key variable to ...
Evapotranspiration is one of the major components of the water balance and has been identified as a key factor in hydrological modelling. For this reason, several methods have been developed to calcul...
First results are shown of a project aiming to estimate daily values of reference crop evapotranspiration ET0 from geo-stationary satellite imagery. In particular, for Woreta, a site in the Ethiopian ...
Evapotranspiration (ET) was estimated from 1981–2005 over Wushen County located in the Mu Us Sandland, China, by applying the Advection-Aridity model, which is based on the complementary relationship ...
The Chinese Loess Plateau is located in the north of China and has a significant impact on the climate and ecosystem evolvement over the East Asian continent. Estimates of evapotranspiration (ET) at a...
In this paper water-balance studies of a soil column at an observation site at Ulvsunda, Stockholm, are reported. The change of the water storage in the soil was obtained from soil moisture measurem...
The paper describes the results of estimations of potential evapotranspiration (ED) in Iceland using Penman's equation. The calculations are based on distribution maps for global radiation for the p...
The ratio of leaf area to ground area required for maintaining potential cvaporation has been studied in a 4-year investigation, and the influence of leaf area index on the water use and the actual ...
This article is based on the thesis, that when sun radiation is not in cxcess and advected energy supply can be neglected, then for periods of plant cover and growth, both evapotranspiration and pla...
A model for calculating thc daily actual evapotranspiration based on tlie potential one is presented. The potcntial evapotranspiration is reduced according to vegetation density, water contcnt in th...
Hourly values of evapotranspiration (ET) for the months July to September 1976 and 1977 were calculated from energy balance measurements at two test sites near the village of Obergurgl in the Austri...
The potential evapotranspiration ETP can be estimated by using Brochet and Gerbier's formula (1972), which is derived from Penman's equation where m and n are tabulated coefficients depending on sea...

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