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Analytical Solution of the Linearized Boussinesq Equation Considering Time-Dependent Downslope Boundary, Variable Recharge and Bedrock Seepage
The present study proposes an analytical solution to a linearized Boussinesq equation considering unsteady downslope river stage, spatio-temporal...
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A Computationally Efficient Method to Determine the Probability of Rainfall-Triggered Cut Slope Failure Accounting for Upslope Hydrological Conditions
We present a new computationally efficient methodology to estimate the probability of rainfall-induced slope failure based on mechanical...
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Effects of hillslope geometry on soil moisture deficit and base flow using an excess saturation model
Estimation of watersheds base flow as a component of subsurface runoff is of significant importance, in particular, in watersheds of high...
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Spatial–temporal analysis of landslides in complex hillslopes of catchments using Dynamic Topmodel
Hillslopes of the catchments in nature have three forms (convergent, divergent, parallel) in terms of plan shape and also in terms of floor curvature...
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Development of the Nash instantaneous unit hydrograph to predict subsurface flow in catchments
For many permeable catchments with proper plant cover, subsurface flows play a key role in generating surface runoff. In this regard, develo**...
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Soil moisture response to land use and topography across a semi-arid watershed: Implications for vegetation restoration on the Chinese Loess Plateau
Soil moisture is a limiting factor of ecosystem development in the semi-arid Loess Plateau. Characterizing the soil moisture response to its dominant...
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Separation of surface flow from subsurface flow in catchments using runoff coefficient
Separating surface flow (SF) from subsurface flow (SSF) based on direct runoff measurements in river gauges is an important issue in hydrology. In...
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Temperature controls diel oscillation of the CO2 concentration in a desert soil
The diel dynamic of the CO 2 concentration in soils in relation to temperature is not yet fully understood. Air temperature might control the soil CO 2 ...
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Prediction of the subsurface flow of hillslopes using a subsurface time-area model
Prediction of subsurface flow (SF) in hillslopes is more complicated than prediction of surface flow; hence, a simple and practical SF model would...
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Distributed Hydrological Models
Physically based distributed hydrological models (PBDHMs), the development of which has been facilitated by advancements in GIS and remote sensing,...
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Hydrological Cycles, Models, and Applications to Forecasting
This chapter presents an overview of hydrology, water cycle, land surface processes (e.g., precipitation, snow, glaciers and frozen soils,...
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Distributed Hydrological Models
Physically based distributed hydrological models (PBDHMs), the development of which has been facilitated by advancements in GIS and remote sensing,...
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A low-dimensional subsurface model for saturated and unsaturated flow processes: ability to address heterogeneity
A low-dimensional model that describes both saturated and unsaturated flow processes in a single equation is presented. Subsurface flow processes in...
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Evaluation of spring discharge dynamics using recession curve analysis: a case study in data-scarce region, Lesser Himalayas, India
There is a huge concern that the springs originating naturally from unconfined aquifers which are the main sources of domestic water on mountainous...
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Hydrological Cycles, Models and Applications to Forecasting
This chapter presents an overview of hydrology, water cycle, land surface processes (e.g., precipitation, snow, glaciers and frozen soils,...
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Numerical analysis on influence of principal parameters of topography on hillslope instability in a small catchment
This study was conducted to identify the influence of three principal parameters constituting topography (slope inclination, soil depth, and slope...
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Groundwater Fluctuations in Slo** Aquifers Induced by Time-Varying Replenishment and Seepage from a Uniformly Rising Stream
This paper analyses the classical problem of transient surface–groundwater interaction in a stream–aquifer system under rather realistic conditions....
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Understanding the dynamics of high and low spring flow: a key to managing the water resources in a small urbanized hillslope of Lesser Himalaya, India
Water scarcity is becoming a major problem in High Mountain Basins of Indian Himalaya. Access to fresh water becomes a core concern for every dweller...
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Response of an Unconfined Slo** Aquifer to Constant Recharge and Seepage from the Stream of Varying Water Level
This paper presents analytical solution of one-dimensional linearized Boussinesq equation characterizing unsteady groundwater flow in an unconfined...