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 Boundary layer entrainment is a critical, much studied, yet relatively poorly understood element of the dynamics of the atmospheric boundary layer. The entrainment fluxes of heat and moisture across the capping inversion strongly affect both the dynamics and cloud structure within the boundary layer. The chief objective of the present grant is to better understand the physical processes which control the rate of this en...
The long term-goal of this project is to provide an improved description and understanding of the ef...
International audienceThe conditional sampling of coherent structures in large-eddy simulations of t...
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 ...
Entrainment in stratocumulus-topped planetary boundary layers is one of the most challenging problem...
Large-eddy simulations of the atmospheric boundary layer have been performed over a range of stabili...
The convective boundary layer (CBL) is the lowest part of the atmosphere. The turbulent motions in t...
Several approaches to parameterize the turbulent transport of momentum, heat, water vapour and cloud...
The reported study examines the dynamics of entrainment and its effects on the evolution of the dry ...
The atmospheric convective boundary layer has been studied for over thirty years in order to underst...
The role of shear in the development and maintenance of a convective boundary layer is studied by me...
Turbulent entrainment is a process of primary importance in the atmospheric boundary layer; however ...
Abstract. This paper compares a number of one-dimensional closure models for the planetary boundary ...
Lack of resolution is a common problem hampering the use of large eddy simulation models for investi...
The long term-goal of this project is to provide an improved description and understanding of the ef...
International audienceThe conditional sampling of coherent structures in large-eddy simulations of t...
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 ...
Entrainment in stratocumulus-topped planetary boundary layers is one of the most challenging problem...
Large-eddy simulations of the atmospheric boundary layer have been performed over a range of stabili...
The convective boundary layer (CBL) is the lowest part of the atmosphere. The turbulent motions in t...
Several approaches to parameterize the turbulent transport of momentum, heat, water vapour and cloud...
The reported study examines the dynamics of entrainment and its effects on the evolution of the dry ...
The atmospheric convective boundary layer has been studied for over thirty years in order to underst...
The role of shear in the development and maintenance of a convective boundary layer is studied by me...
Turbulent entrainment is a process of primary importance in the atmospheric boundary layer; however ...
Abstract. This paper compares a number of one-dimensional closure models for the planetary boundary ...
Lack of resolution is a common problem hampering the use of large eddy simulation models for investi...
The long term-goal of this project is to provide an improved description and understanding of the ef...
International audienceThe conditional sampling of coherent structures in large-eddy simulations of t...
thesisNegatively buoyant forces in the stable boundary layer (SBL) damp turbulent motions, resulting...