The flow past heated topography is examined with both linear and nonlinear models. It is first shown that the forcing of an obstacle with horizontally homogenous surface heating can be approximated by the forcing of an obstacle with surface heating isolated over the obstacle. The small-amplitude flow past an obstacle with isolated heating is then examined with a linear model. Under the linear approximation, the flow response to heated topography is simply the addition of the separate responses to thermal and orographic forcing. These separate responses are first considered individually and then the combined response is examined. Nondimensional parameters are developed that measure the relative importance of thermal and orographic forcing. N...
Summary. — A new approximate analysis is presented for stably stratified flows at low Froude number ...
Thermal convection of a Boussinesq fluid in a layer confined between two infinite horizontal walls i...
Abstract The complete day–night cycle of the circulation over a slope under simplifie...
This is the publisher's version, also available electronically from http://journals.ametsoc.org/doi/...
This paper reviews the current understanding of moist orographic convection and its regulation by su...
The present study investigates basic aspects of the flow of a density-stratified fluid past three-di...
This is the publisher's version, also available electronically from http://journals.ametsoc.org/doi/...
The air¯ow over an idealized orography with two mountain peaks and a valley between is investigated ...
The validity of linear smoothing of topography for numerical weather prediction and the variation of...
ABSTRACT: In mountainous terrain, landscape strongly influences the thermal state of snow. An energy...
A laboratory study was conducted in order to gain an understanding of thermal convection in a comple...
A laboratory study was conducted in order to gain an understanding of thermal convection in a comple...
By means of a large-eddy simulation, the convective boundary layer is investigated for flows over wa...
Recently, models of regional heat and moisture fluxes in terrain with bluff roughness elements have ...
Graduation date: 2004A modeling study is undertaken to better understand the physics of\ud katabatic...
Summary. — A new approximate analysis is presented for stably stratified flows at low Froude number ...
Thermal convection of a Boussinesq fluid in a layer confined between two infinite horizontal walls i...
Abstract The complete day–night cycle of the circulation over a slope under simplifie...
This is the publisher's version, also available electronically from http://journals.ametsoc.org/doi/...
This paper reviews the current understanding of moist orographic convection and its regulation by su...
The present study investigates basic aspects of the flow of a density-stratified fluid past three-di...
This is the publisher's version, also available electronically from http://journals.ametsoc.org/doi/...
The air¯ow over an idealized orography with two mountain peaks and a valley between is investigated ...
The validity of linear smoothing of topography for numerical weather prediction and the variation of...
ABSTRACT: In mountainous terrain, landscape strongly influences the thermal state of snow. An energy...
A laboratory study was conducted in order to gain an understanding of thermal convection in a comple...
A laboratory study was conducted in order to gain an understanding of thermal convection in a comple...
By means of a large-eddy simulation, the convective boundary layer is investigated for flows over wa...
Recently, models of regional heat and moisture fluxes in terrain with bluff roughness elements have ...
Graduation date: 2004A modeling study is undertaken to better understand the physics of\ud katabatic...
Summary. — A new approximate analysis is presented for stably stratified flows at low Froude number ...
Thermal convection of a Boussinesq fluid in a layer confined between two infinite horizontal walls i...
Abstract The complete day–night cycle of the circulation over a slope under simplifie...