Abstract. A new formulation for the turbulence dissipa-tion rate ε occurring in meandering conditions has been pre-sented. The derivation consists of a MacLaurin series expan-sion of a lateral dispersion parameter that represents cases in which turbulence and oscillatory movements associated to the meandering events coexist. The new formulation presents the identical physical premises contained in the classical and largely used one, but the new formulation derived from me-andering situations is expressed in terms of the loop param-eter m that controls the absolute value of the negative lobe in the meandering autocorrelation function. Therefore, the m magnitude regulates the turbulence dissipation rate. This dis-sipation rate decreases for c...
The phenomenon known as meandering describes the unsteady trajectory variations of the wake of a win...
Eulerian and Lagrangian statistics in the atmospheric convective boundary layer (CBL) are studied by...
The periods of time-varying turbulence in the atmospheric boundary layer, i.e.\ the morning and even...
International audienceA new formulation for the turbulence dissipation rate ? occurring in meanderin...
An alternative formulation for the low wind speed-meandering autocorrelation function is presented. ...
A Lagrangian stochastic particle model driven by observed winds from a net-work of 13 sonic anemomet...
Abstract: A turbulent scalar transport model is proposed which is based on the analytical framework ...
A new theoretical model has been developed to predict the transport of atmospheric pollutants as the...
In this paper a set of new Reynolds averaged equations which contain both the dissipation and disper...
New Reynolds mean momentum equations including turbulent viscosity and dispersion are used to analyz...
The statistics describing variations of turbulent motions within the so called inertial range of len...
This study is a contribution toward the understanding and prediction of turbulent dispersion of poll...
Conselho Nacional de Desenvolvimento Científico e TecnológicoThis study employed different autocorre...
NOUS PRESENTONS DES RESULTATS EXPERIMENTAUX CONCERNANT LA DISPERSION DE TRACEURS PASSIFS DANS DES EX...
Graduation date: 1994The statistics describing variations of turbulent motions within the so called\...
The phenomenon known as meandering describes the unsteady trajectory variations of the wake of a win...
Eulerian and Lagrangian statistics in the atmospheric convective boundary layer (CBL) are studied by...
The periods of time-varying turbulence in the atmospheric boundary layer, i.e.\ the morning and even...
International audienceA new formulation for the turbulence dissipation rate ? occurring in meanderin...
An alternative formulation for the low wind speed-meandering autocorrelation function is presented. ...
A Lagrangian stochastic particle model driven by observed winds from a net-work of 13 sonic anemomet...
Abstract: A turbulent scalar transport model is proposed which is based on the analytical framework ...
A new theoretical model has been developed to predict the transport of atmospheric pollutants as the...
In this paper a set of new Reynolds averaged equations which contain both the dissipation and disper...
New Reynolds mean momentum equations including turbulent viscosity and dispersion are used to analyz...
The statistics describing variations of turbulent motions within the so called inertial range of len...
This study is a contribution toward the understanding and prediction of turbulent dispersion of poll...
Conselho Nacional de Desenvolvimento Científico e TecnológicoThis study employed different autocorre...
NOUS PRESENTONS DES RESULTATS EXPERIMENTAUX CONCERNANT LA DISPERSION DE TRACEURS PASSIFS DANS DES EX...
Graduation date: 1994The statistics describing variations of turbulent motions within the so called\...
The phenomenon known as meandering describes the unsteady trajectory variations of the wake of a win...
Eulerian and Lagrangian statistics in the atmospheric convective boundary layer (CBL) are studied by...
The periods of time-varying turbulence in the atmospheric boundary layer, i.e.\ the morning and even...