Internal wave coupling processes in Earth's atmosphere
E Yiğit, AS Medvedev - Advances in Space Research, 2015 - Elsevier
This paper presents a contemporary review of vertical coupling in the atmosphere and
ionosphere system induced by internal waves of lower atmospheric origin. Atmospheric …
ionosphere system induced by internal waves of lower atmospheric origin. Atmospheric …
Overview of nighttime ionospheric instabilities at low-and mid-latitudes: Coupling aspects resulting in structuring at the mesoscale
We present a review of the current state of understanding regarding two classes of
irregularities causing mesoscale structuring (hundreds of kilometers) in the nighttime …
irregularities causing mesoscale structuring (hundreds of kilometers) in the nighttime …
A global view of stratospheric gravity wave hotspots located with Atmospheric Infrared Sounder observations
L Hoffmann, X Xue… - Journal of Geophysical …, 2013 - Wiley Online Library
The main aim of this study is to find and classify hotspots of stratospheric gravity waves on a
global scale. The analysis is based on a 9 year record (2003 to 2011) of radiance …
global scale. The analysis is based on a 9 year record (2003 to 2011) of radiance …
Generation of large‐scale gravity waves and neutral winds in the thermosphere from the dissipation of convectively generated gravity waves
SL Vadas, H Liu - Journal of Geophysical Research: Space …, 2009 - Wiley Online Library
We study the response of the thermosphere and ionosphere to the dissipation of gravity
waves (GWs) excited by a deep convective plume on 1 October 2005 at 52.5° W, 15.0° S …
waves (GWs) excited by a deep convective plume on 1 October 2005 at 52.5° W, 15.0° S …
Sources of the traveling ionospheric disturbances observed by the ionospheric TIDDBIT sounder near Wallops Island on 30 October 2007
SL Vadas, G Crowley - Journal of Geophysical Research …, 2010 - Wiley Online Library
We model the gravity waves (GWs) excited by Tropical Storm (TS) Noel at 0432 UT on 30
October 2007. Using forward ray tracing, we calculate the body forces which result from the …
October 2007. Using forward ray tracing, we calculate the body forces which result from the …
Simultaneous observation of ionospheric plasma bubbles and mesospheric gravity waves during the SpreadFEx Campaign
During the Spread F Experiment campaign, under NASA Living with a Star (LWS) program,
carried out in the South American Magnetic Equator region from 22 September to 8 …
carried out in the South American Magnetic Equator region from 22 September to 8 …
Concentric gravity waves in the mesosphere generated by deep convective plumes in the lower atmosphere near Fort Collins, Colorado
J Yue, SL Vadas, CY She, T Nakamura… - Journal of …, 2009 - Wiley Online Library
Gravity waves in the mesopause region (80–105 km) may induce perturbations in OH
Meinal Band emissions at∼ 87 km. These perturbations can be observed by ground‐based …
Meinal Band emissions at∼ 87 km. These perturbations can be observed by ground‐based …
Numerical modeling of the large‐scale neutral and plasma responses to the body forces created by the dissipation of gravity waves from 6 h of deep convection in …
SL Vadas, HL Liu - Journal of Geophysical Research: Space …, 2013 - Wiley Online Library
We study the response of the thermosphere and ionosphere to gravity waves (GWs) excited
by 6 h of deep convection in Brazil on the evening of 01 October 2005 via the use of …
by 6 h of deep convection in Brazil on the evening of 01 October 2005 via the use of …
Characteristics of the quiet‐time hot spot gravity waves observed by GOCE over the Southern Andes on 5 July 2010
We analyze quiet‐time data from the Gravity Field and Ocean Circulation Explorer satellite
as it overpassed the Southern Andes at z≃ 275 km on 5 July 2010 at 23 UT. We extract the …
as it overpassed the Southern Andes at z≃ 275 km on 5 July 2010 at 23 UT. We extract the …
Secondary gravity waves from the stratospheric polar vortex over ALOMAR observatory on 12–14 January 2016: observations and modeling
We analyze the gravity waves (GWs) observed by a Rayleigh lidar at the Arctic Lidar
Observatory for Middle Atmosphere Research (ALOMAR)(16.08° E, 69.38° N) in Norway at …
Observatory for Middle Atmosphere Research (ALOMAR)(16.08° E, 69.38° N) in Norway at …