Gravity waves are known to transport energy and momentum to the middle atmosphere. The breaking processes associated with divergence of fluxes of energy and momentum into the atmosphere occur on scales that cannot be resolved in models and therefore have to be parameterized. The question remains as to whether it is possible to use a turbulence model on scales below 100 m and what kind of turbulence model should that be. Here we use high spatial resolution observations of the OH nightglow located near 90‐km altitude from the Nordic Optical Telescope to observe quasiperiodic structures down to horizontal scales of 4.5 m. These results indicate that a Kolmogorov type of energy cascade model of turbulence with a −5/3 power law appears to be sat...
A 2-D nonlinear compressible model is used to simulate a large-amplitude, multiscale mountain wave e...
We present a new version of the HIgh Altitude Mechanistic general Circulation Model (HIAMCM) with sp...
International audienceAtmospheric motions are governed by turbulent motions associated to non-trivi...
The atmospheric energy spectrum as a function of horizontal wavenumber over the range from a few kil...
Midlatitude fluctuations of the atmospheric winds on scales of thousands of kilometers, the most ene...
A new version of the Fast Airglow Imager (FAIM) for the detection of atmospheric waves in the OH air...
International audienceAircraft measurements of the power spectra of the horizontal wind field typica...
International audienceClassically, turbulence has been modeled by a hierarchy of different isotropic...
A new version of the Fast Airglow Imager (FAIM) for the detection of atmospheric waves in the OH air...
International audienceIn this first of a three-part series, we argue that the dynamics of turbulence...
Gravity waves (disturbances to the density structure of the atmosphere whose restoring forces are gr...
The classical energy cascade in turbulence as described by Richardson and Kolmogorov is predominantl...
We analyzed 286 nights of data from the OH* airglow imager FAIM 3 (Fast Airglow IMager) acquired at ...
We analysed 286 nights of data from the OH* airglow imager FAIM 3 (Fast Airglow IMager) acquired at ...
A mesospheric model of the airglow emission is developed to recover the night variations observed at...
A 2-D nonlinear compressible model is used to simulate a large-amplitude, multiscale mountain wave e...
We present a new version of the HIgh Altitude Mechanistic general Circulation Model (HIAMCM) with sp...
International audienceAtmospheric motions are governed by turbulent motions associated to non-trivi...
The atmospheric energy spectrum as a function of horizontal wavenumber over the range from a few kil...
Midlatitude fluctuations of the atmospheric winds on scales of thousands of kilometers, the most ene...
A new version of the Fast Airglow Imager (FAIM) for the detection of atmospheric waves in the OH air...
International audienceAircraft measurements of the power spectra of the horizontal wind field typica...
International audienceClassically, turbulence has been modeled by a hierarchy of different isotropic...
A new version of the Fast Airglow Imager (FAIM) for the detection of atmospheric waves in the OH air...
International audienceIn this first of a three-part series, we argue that the dynamics of turbulence...
Gravity waves (disturbances to the density structure of the atmosphere whose restoring forces are gr...
The classical energy cascade in turbulence as described by Richardson and Kolmogorov is predominantl...
We analyzed 286 nights of data from the OH* airglow imager FAIM 3 (Fast Airglow IMager) acquired at ...
We analysed 286 nights of data from the OH* airglow imager FAIM 3 (Fast Airglow IMager) acquired at ...
A mesospheric model of the airglow emission is developed to recover the night variations observed at...
A 2-D nonlinear compressible model is used to simulate a large-amplitude, multiscale mountain wave e...
We present a new version of the HIgh Altitude Mechanistic general Circulation Model (HIAMCM) with sp...
International audienceAtmospheric motions are governed by turbulent motions associated to non-trivi...