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The complementary relationship (CR) between potential evaporation (LEp) and actual evaporation (LE) is widely used to explainthe evaporation paradox and to estimate LE, in which wet environment evapor...
In Douala, economic capital of Cameroon, annual rainfall and temperature from its meteorological station (latitude: 4o00'N; longitude: 9o43'E; elevation: 5.0 m) were obtained and analysed to investiga...
To determine the effects of land use on groundwater quality in Western Australia, a quantitative analysis is carried out using groundwater quality data supplied by the Department of Water from over 50...
Based on Reanalysis datasets from National Centers for Environmental Prediction/National Center for Atmospheric Research (NCEP/NCAR) and summer rainfall datasets from China National Climate Center (NC...
Geoelectrical soundings using the Schlumberger array were carried out in the vicinity of 23 pumping test sites to determine aquifer parameters, central Jordan. On the basis of aquifer geometry, the ar...
In the complementary relationship (CR) between actual and potential evapotranspiration, wet environment evapotranspiration (Ew) is usually calculatedusing the Priestley-Taylor (P-T) equation. Based on...
The Budyko, Bouchet, and Penman hypothesestogether describe, using different formulae, the tightconnections and feedbacks between water energy balances and the landscape. The discrepancy between th...
The red tides often occurred in the estuaries and near sea in recent years. Prediction of occurrence of this phenomenon has been an important issue in the East Asian countries. This paper develops a c...
A simulation study was performed to analyze the relationship between the volume of moisture stored in a soil profile and the rate of percolation and subsurface return flow. The simulation study was de...

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