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Soil erosion is a crucial problem in Nepal where more than 80% of the land area is mountainous. In this study, two commonly used empirical soil erosion models, Revised Universal Soil Loss Equation (RU...
Soil erosion is a crucial problem in Nepal where more than 80% of the land area is mountainous. In this study, two commonly used empirical soil erosion models, Revised Universal Soil Loss Equation (RU...
A 112 square kilometer research watershed was instrumented to study basic hydrologic processes in the mountainous areas of the N,ortheastern United States. Within this area the rainfall-runoff relat...
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...
The standard error of mean areal rainfall was calculated for various densities of rain gauge network in a small mountainous watershed in the summer of 1978. It is shown that a) the optimum gauge den...
Landsat-5 Thematic Mapper (TM) reflectances recorded i May 1989 from a mountainous catchment at Kvikne, Norway, are analyzed and compared with simultaneously measured in situ albedo. The satellite-r...
The orographic and temporal gradients of rainfall in a mountainous watershed in southwestcrfi British Columbia have been analyzed and streamflow has been estimated using a watershed model. The study...
In a snowy watershed, the response of streamwater chemistry to snowmelt depends not only on meltwater chemistry but on the hydrochemical processes of the subsurface water. In this study, the δ18O valu...
A three-layer TOPMODEL is constructed by integrating diffusion wave approach into surface flow, soil moisture deficit into inter flow and exponential recession curve function into base flow. A subtrop...
The Generalized Likelihood Uncertainty Estimation (GLUE) is here incorporated into a deterministic landslide model (SHALSTAB) to generate 4000 landslide susceptibility maps which enclose various combi...

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