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Erosion Predictions by Empirical Models in a Mountainous Watershed in Nepal
Erosion Predictions Empirical Models Mountainous Watershed Nepal
2015/8/14
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...
Rainfall-Runoff Characteristics for a Mountainous Watershed in the Northeast United States
Rainfall-Runoff Characteristics Mountainous Watershed Northeast United States
2009/10/28
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...
Measurement and Mapping of Potential Evapotranspiration in a Small Mountainous Watershed
Measurement Mapping Potential Evapotranspiration Small Mountainous Watershed
2009/10/28
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...
Assessment of True Variability of Small Rainfall Events in a Small Mountainous Watershed in the Summer
Assessment True Variability Small Rainfall Events Mountainous Watershed
2009/10/28
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...
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...
Response Time of Forested Mountainous Watersheds in Humid Regions
Response Time Forested Mountainous Watersheds Humid Regions
2009/10/23
This study proposes an analytical method for the estimation of time lag for forested mountainous watersheds. The water flow in a watershed is separated and analyzed in two phases, the land or hillslop...
THE PREDICTION OF DAILY OUTFLOW FOR AN UNGAGED MOUNTAINOUS BASIN
DAILY OUTFLOW rainfall period Generalized Flood Pattern Method
2009/10/19
To evaluate the daily outflow from a 212-km2 basin in a mountainous part of the downstream Amur river, which has no rain gages, a modeling approach is needed. The average basin rainfall during a rainf...