Our long term goals are to understand the dynamics of atmospheric motions on scales of order 10 m-10 km in sufficient detail to be able to provide a consistent subgrid scale turbulent closure for models across a range of scales, and to be able to utilize simulated variances as a measure of forecast predictability. OBJECTIVES The chief objective of the present grant is to better understand the physical processes which control the rate of entrainment fluxes of heat and moisture across the capping inversion of the atmospheric boundary layer, and to formulate a closure model for cloud-top entrainment that is consistent for a broad range of boundary layer conditions and forcings. Ideally, this closure model would allow one to produce a simulatio...
We derive the turbulent structure parameters of temperature C 2 T and humidity C 2 q from high-resol...
The long term-goal of this project is to provide an improved description and understanding of the ef...
thesisNegatively buoyant forces in the stable boundary layer (SBL) damp turbulent motions, resulting...
Our long term goals are to understand the dynamics of atmospheric motions on scales of order 10 m-10...
The use of large eddy simulation, or LES, to study the atmospheric boundary layer dates back to the ...
Large-eddy simulations of the atmospheric boundary layer have been performed over a range of stabili...
Several approaches to parameterize the turbulent transport of momentum, heat, water vapour and cloud...
Abstract. This paper compares a number of one-dimensional closure models for the planetary boundary ...
Entrainment in stratocumulus-topped planetary boundary layers is one of the most challenging problem...
Several approaches to parameterize the turbulent transport of momentum, heat, water vapour and cloud...
The role of shear in the development and maintenance of a convective boundary layer is studied by me...
The convective boundary layer (CBL) is the lowest part of the atmosphere. The turbulent motions in t...
The authors use large-eddy simulation (LES) to investigate entrainment and structure of the inversio...
To quantify the turbulent transport at gray zone length scales between 1 and 10 km, the Lagrangian e...
Previous large-eddy simulations (LES) of stratocumulus-topped boundary layers have been exclusively ...
We derive the turbulent structure parameters of temperature C 2 T and humidity C 2 q from high-resol...
The long term-goal of this project is to provide an improved description and understanding of the ef...
thesisNegatively buoyant forces in the stable boundary layer (SBL) damp turbulent motions, resulting...
Our long term goals are to understand the dynamics of atmospheric motions on scales of order 10 m-10...
The use of large eddy simulation, or LES, to study the atmospheric boundary layer dates back to the ...
Large-eddy simulations of the atmospheric boundary layer have been performed over a range of stabili...
Several approaches to parameterize the turbulent transport of momentum, heat, water vapour and cloud...
Abstract. This paper compares a number of one-dimensional closure models for the planetary boundary ...
Entrainment in stratocumulus-topped planetary boundary layers is one of the most challenging problem...
Several approaches to parameterize the turbulent transport of momentum, heat, water vapour and cloud...
The role of shear in the development and maintenance of a convective boundary layer is studied by me...
The convective boundary layer (CBL) is the lowest part of the atmosphere. The turbulent motions in t...
The authors use large-eddy simulation (LES) to investigate entrainment and structure of the inversio...
To quantify the turbulent transport at gray zone length scales between 1 and 10 km, the Lagrangian e...
Previous large-eddy simulations (LES) of stratocumulus-topped boundary layers have been exclusively ...
We derive the turbulent structure parameters of temperature C 2 T and humidity C 2 q from high-resol...
The long term-goal of this project is to provide an improved description and understanding of the ef...
thesisNegatively buoyant forces in the stable boundary layer (SBL) damp turbulent motions, resulting...