Mesosphere inversion layers and stratosphere temperature enhancements
JW Meriwether, AJ Gerrard - Reviews of Geophysics, 2004 - Wiley Online Library
It has been known for at least 30 years that vertically narrow thermal layers form within the
middle atmosphere. Two types of temperature enhancements, the low‐latitude to midlatitude …
middle atmosphere. Two types of temperature enhancements, the low‐latitude to midlatitude …
A review of the mesosphere inversion layer phenomenon
JW Meriwether, CS Gardner - Journal of Geophysical …, 2000 - Wiley Online Library
An active topic of current research in aeronomy is the study of the dynamics of the
mesosphere and lower thermosphere (MLT) from 60 to 130 km, especially in regard to the …
mesosphere and lower thermosphere (MLT) from 60 to 130 km, especially in regard to the …
Alpine soil temperature variability at multiple scales
The functioning of ecosystems is strongly correlated to soil temperature dynamics. Because
only a few studies so far have investigated the spatio-temporal variability of alpine soil …
only a few studies so far have investigated the spatio-temporal variability of alpine soil …
Recent observations of mesospheric temperature inversions
T Leblanc, A Hauchecorne - Journal of Geophysical Research …, 1997 - Wiley Online Library
The recent results of observed mesospheric temperature inversions are presented. Using
two Rayleigh lidars (located in the south of France) and ISAMS (Improved Stratospheric And …
two Rayleigh lidars (located in the south of France) and ISAMS (Improved Stratospheric And …
Gravity waves in the mesosphere generated by tropospheric convention
JR Holton, MJ Alexander - Tellus B, 1999 - Wiley Online Library
The observed cold temperatures in the summer mesosphere are dynamically maintained
primarily through upwelling induced in response to the action of a zonal drag force caused …
primarily through upwelling induced in response to the action of a zonal drag force caused …
Local mean state changes due to gravity wave breaking modulated by the diurnal tide
During gravity wave breaking, heating rates are determined by wave advection, turbulent
diffusion, and turbulence dissipative heating. A series of numerical experiments show that …
diffusion, and turbulence dissipative heating. A series of numerical experiments show that …
Gravity wave dynamics in a mesospheric inversion layer: 1. Reflection, trapping, and instability dynamics
DC Fritts, B Laughman, L Wang… - Journal of …, 2018 - Wiley Online Library
An anelastic numerical model is employed to explore the dynamics of gravity waves (GWs)
encountering a mesosphere inversion layer (MIL) having a moderate static stability …
encountering a mesosphere inversion layer (MIL) having a moderate static stability …
Evaluation of optimization of lidar temperature analysis algorithms using simulated data
T Leblanc, IS McDermid… - Journal of …, 1998 - Wiley Online Library
Temperature lidar data have been simulated in order to test the Jet Propulsion Laboratory
(JPL) SO3ANL version 3.2 and Service d'Aeronomie du Centre National de la Recherche …
(JPL) SO3ANL version 3.2 and Service d'Aeronomie du Centre National de la Recherche …
Modelling spatio-temporal near-surface temperature variation in high mountain landscapes
A surface energy balance model (SEB), describing the fluxes of latent and sensible heat as
well as the ground heat flux at different surfaces, was developed to simulate substrate …
well as the ground heat flux at different surfaces, was developed to simulate substrate …
Simultaneous observations of a Mesospheric Inversion Layer and turbulence during the ECOMA-2010 rocket campaign
A Szewczyk, B Strelnikov, M Rapp… - Annales …, 2013 - angeo.copernicus.org
From 19 November to 19 December 2010 the fourth and final ECOMA rocket campaign was
conducted at Andøya Rocket Range (69° N, 16° E) in northern Norway. We present and …
conducted at Andøya Rocket Range (69° N, 16° E) in northern Norway. We present and …