The Boussinesq model for subsurface flow in an idealized sloping aquifer has recently been extended to hillslopes of arbitrary geometry by incorporating the width function w(s) into the governing equation, were x is the distance along the length of the hillslopes. The resulting mathematical model can be simplified if three higher order terms containing (1/w)w’(x) are dropped. In this preliminary report we describe the model along with some characteristic hillslopes that will be used to test it and develop it further
We present a coupling between the one-dimensional Richards equation for vertical unsaturated flow an...
Hillslope response has traditionally been studied by means of the hydraulic groundwater theory. Subs...
Abstract The linearized hillslope Boussinesq equation, introduced by Brutsaert (1994), describes the...
Hillslope response to rainfall remains one of the central problems of catchment hydrology. Flow proc...
Hillslope response to rainfall remains one of the central problems of catchment hydrology. Flow proc...
Hillslope response to rainfall remains one of the central problems of catchment hydrology. Flow proc...
The Boussinesq equation for subsurface flow in an idealized sloping aquifer of unit width has recent...
The Boussinesq equation for subsurface flow in an idealized sloping aquifer of unit width has recent...
We present a coupling between the one-dimensional Richards equation for vertical unsaturated flow an...
Key words: hillslope hydrology, low-dimensional modeling, Boussinesq equation, Richards equation, wa...
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...
In this study the recently introduced hill slope-storage Boussinesq (hsB) model is cast in a general...
Hillslope response has traditionally been studied by means of the hydraulic groundwater theory. Subs...
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...
Hillslope response has traditionally been studied by means of the hydraulic groundwater theory. Subs...
Abstract The linearized hillslope Boussinesq equation, introduced by Brutsaert (1994), describes the...
Hillslope response to rainfall remains one of the central problems of catchment hydrology. Flow proc...
Hillslope response to rainfall remains one of the central problems of catchment hydrology. Flow proc...
Hillslope response to rainfall remains one of the central problems of catchment hydrology. Flow proc...
The Boussinesq equation for subsurface flow in an idealized sloping aquifer of unit width has recent...
The Boussinesq equation for subsurface flow in an idealized sloping aquifer of unit width has recent...
We present a coupling between the one-dimensional Richards equation for vertical unsaturated flow an...
Key words: hillslope hydrology, low-dimensional modeling, Boussinesq equation, Richards equation, wa...
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...
In this study the recently introduced hill slope-storage Boussinesq (hsB) model is cast in a general...
Hillslope response has traditionally been studied by means of the hydraulic groundwater theory. Subs...
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...
Hillslope response has traditionally been studied by means of the hydraulic groundwater theory. Subs...
Abstract The linearized hillslope Boussinesq equation, introduced by Brutsaert (1994), describes the...