Add to ORKG[1] This technical note presents an analytical solution to the linearized hillslope-storage Boussinesq equation for subsurface flow along complex hillslopes with exponential width functions and discusses the application of analytical solutions to storage-based subsurface flow equations in catchment studies. INDEX TERMS: 1829 Hydrology: Groundwate
We present a coupling between the one-dimensional Richards equation for vertical unsaturated flow an...
Hillslopes have complex three-dimensional shapes that are characterized by their plan shape, profile...
Unsaturated flow is an important factor that affects groundwater motion. Among various drainage mode...
This technical note presents an analytical solution to the linearized hillslope-storage Boussinesq e...
Hillslope response to rainfall remains one of the central problems of catchment hydrology. Flow proc...
Abstract The linearized hillslope Boussinesq equation, introduced by Brutsaert (1994), describes the...
Hillslope response has traditionally been studied by means of the hydraulic groundwater theory. Subs...
The linearized hillslope Boussinesq equation, introduced by Brutsaert (1994), describes the dynamics...
Subsurface flow from a hillslope can be described by the hydraulic groundwater theory as formulated ...
The Boussinesq model for subsurface flow in an idealized sloping aquifer has recently been extended ...
The Boussinesq equation for subsurface flow in an idealized sloping aquifer of unit width has recent...
The matter of the efficient and parsimonious parameterization of hillslope subsurface flow remains a...
The matter of the efficient and parsimonious parameterization of hillslope subsurface flow remains a...
This paper presents two analytical solutions of the linearized Boussinesq equation for an inclined a...
In this study the recently introduced hill slope-storage Boussinesq (hsB) model is cast in a general...
We present a coupling between the one-dimensional Richards equation for vertical unsaturated flow an...
Hillslopes have complex three-dimensional shapes that are characterized by their plan shape, profile...
Unsaturated flow is an important factor that affects groundwater motion. Among various drainage mode...
This technical note presents an analytical solution to the linearized hillslope-storage Boussinesq e...
Hillslope response to rainfall remains one of the central problems of catchment hydrology. Flow proc...
Abstract The linearized hillslope Boussinesq equation, introduced by Brutsaert (1994), describes the...
Hillslope response has traditionally been studied by means of the hydraulic groundwater theory. Subs...
The linearized hillslope Boussinesq equation, introduced by Brutsaert (1994), describes the dynamics...
Subsurface flow from a hillslope can be described by the hydraulic groundwater theory as formulated ...
The Boussinesq model for subsurface flow in an idealized sloping aquifer has recently been extended ...
The Boussinesq equation for subsurface flow in an idealized sloping aquifer of unit width has recent...
The matter of the efficient and parsimonious parameterization of hillslope subsurface flow remains a...
The matter of the efficient and parsimonious parameterization of hillslope subsurface flow remains a...
This paper presents two analytical solutions of the linearized Boussinesq equation for an inclined a...
In this study the recently introduced hill slope-storage Boussinesq (hsB) model is cast in a general...
We present a coupling between the one-dimensional Richards equation for vertical unsaturated flow an...
Hillslopes have complex three-dimensional shapes that are characterized by their plan shape, profile...
Unsaturated flow is an important factor that affects groundwater motion. Among various drainage mode...