International audienceA formalism is proposed to represent a broadband spectrum of Gravity Waves (GWs) via the superposition of a large ensemble of statistically independent monochromatic ones. To produce this large ensemble at a reasonable numerical cost, we use the fact that the life cycles of the waves needed to be parameterized in General Circulation Models (GCMs) have time scales that largely exceed the time step of the model. We can therefore launch few waves with characteristics chosen randomly at each time step, and make them having an effect on a longer time scale by applying an AR1 relation between the gravity waves drag at a given time and that at the next time step. The stochastic GW parameterization is applied to a GCM in the t...
Although there is a rich literature on modelling the effects of broad spectrum gravity waves (GW) in...
We present a numerical spectral model (NSM) that describes the equatorial oscillations in the zonal ...
Most of our observational knowledge of gravity waves in the atmosphere comes from vertical profiles ...
International audienceA formalism is proposed to represent a broadband spectrum of Gravity Waves (GW...
Model that includes a well resolved stratosphere. It is based on a stochastic approach, where an ens...
International audienceA formalism is proposed to parameterize the gravity waves due to convection in...
The general circulation of the middle atmosphere, particularly of the mesosphere, is strongly depend...
International audienceLong-range infrasound propagation is controlled by atmospheric waveguides that...
In order to simulate stratospheric phenomena, such as the Quasi-Biennial Oscillation (QBO), atmosphe...
International audienceBased on the theoretical and experimental facts that gravity waves (GWs) can b...
Small-scale gravity waves (GWs) with horizontal wavelengths of tens up to several hundred kilometers...
Characteristic properties of gravity waves from convection over the continental United States are de...
Orographic gravity waves (OGWs) are ubiquitous in the atmosphere and they have an important influenc...
Previous versions of GISS climate models have either used formulations of Rayleigh drag to represent...
The impact of optimal parameters in a non-orographic gravity wave drag parameterization on the middl...
Although there is a rich literature on modelling the effects of broad spectrum gravity waves (GW) in...
We present a numerical spectral model (NSM) that describes the equatorial oscillations in the zonal ...
Most of our observational knowledge of gravity waves in the atmosphere comes from vertical profiles ...
International audienceA formalism is proposed to represent a broadband spectrum of Gravity Waves (GW...
Model that includes a well resolved stratosphere. It is based on a stochastic approach, where an ens...
International audienceA formalism is proposed to parameterize the gravity waves due to convection in...
The general circulation of the middle atmosphere, particularly of the mesosphere, is strongly depend...
International audienceLong-range infrasound propagation is controlled by atmospheric waveguides that...
In order to simulate stratospheric phenomena, such as the Quasi-Biennial Oscillation (QBO), atmosphe...
International audienceBased on the theoretical and experimental facts that gravity waves (GWs) can b...
Small-scale gravity waves (GWs) with horizontal wavelengths of tens up to several hundred kilometers...
Characteristic properties of gravity waves from convection over the continental United States are de...
Orographic gravity waves (OGWs) are ubiquitous in the atmosphere and they have an important influenc...
Previous versions of GISS climate models have either used formulations of Rayleigh drag to represent...
The impact of optimal parameters in a non-orographic gravity wave drag parameterization on the middl...
Although there is a rich literature on modelling the effects of broad spectrum gravity waves (GW) in...
We present a numerical spectral model (NSM) that describes the equatorial oscillations in the zonal ...
Most of our observational knowledge of gravity waves in the atmosphere comes from vertical profiles ...