Ultrafast Kelvin waves in the MLT airglow and wind, and their interaction with the atmospheric tides [PDF]
Airglow and wind measurements from the Brazilian equatorial region were used to investigate the presence and the effects of the 3–4-day ultrafast Kelvin waves in the MLT.
F. Egito +3 more
doaj +4 more sources
Airglow and Aurorae at Dome A, Antarctica [PDF]
Despite the absence of artificial light pollution at Antarctic plateau sites such as Dome A, other factors such as airglow, aurorae, and extended periods of twilight have the potential to adversely affect optical observations. We present a statistical analysis of the airglow and aurorae at Dome A using spectroscopic data from Nigel, an optical/near-IR ...
Sims, Geoff +20 more
openaire +3 more sources
Space-Based Limb-Imaging Spectrometer for Atmospheric O2 Airglow Detection
This paper presents a space-based limb-imaging spectrometer (LIS) for detecting atmospheric O2 airglow; it scans the atmosphere with a vertical range of 10–100 km and has a vertical resolution of 2 km. The LIS’s detection performance needs to be examined
Minjie Zhao +14 more
doaj +2 more sources
Quasi 6‐Day Wave Variability in the Thermosphere and Ionosphere: Observations and Modeling
Satellite observations of the upper mesosphere and lower thermosphere from TIMED‐SABER and ICON‐MIGHTI reveal a clear Quasi 6‐Day Wave (Q6DW) event in the winds and temperatures in this region.
Oluwafisayo P. Owolabi +2 more
doaj +2 more sources
Post‐sunset equatorial plasma bubble (EPB) formation is believe to be influenced by factors including thermospheric neutral winds. This study characterizes pre‐sunset neutral winds observed by ICON on EPB occurrences observed by GOLD over the east ...
V. J. Adkins +2 more
doaj +2 more sources
HF pump-induced electron heating and artificial airglow at high latitudes: Aspect angle dependence [PDF]
Large electron temperature increases (~3000 K) in the ionospheric F-region, produced by powerful HF wave injection, were measured using the EISCAT incoherent scatter radar near Tromsø, Norway, on 7 October 1999.
Rietveld, M. T. +4 more
core +4 more sources
On the location and structure of the artificial 630-nm airglow patch over Sura facility [PDF]
International audienceResults are presented of the artificial optical emission of the atomic oxygen red line (the radiation of level O(1D) with a wavelength of 630 nm) from the HF-pumped ionosphere, obtained in September 2004 at the SURA heating facility
Atroshenko, M. A. +11 more
core +2 more sources
The first coordinated observations of mid-latitude E-region quasi-periodic radar echoes and lower thermospheric 557.7-nm airglow [PDF]
We present the first coordinated observations of quasi-periodic (QP) radar echoes from sporadic-E (Es) field-aligned irregularities (FAIs), OI 557.7-nm airglow, and neutral winds in a common volume over Shigaraki, Japan (34.9° N, 136.1° E) on the ...
T. Ogawa +4 more
doaj +1 more source
Computing uncertainties in ionosphere‐airglow models: II. The Martian airglow [PDF]
One of the objectives of spectrometers onboard space missions is to retrieve atmospheric parameters (notably density, composition and temperature). To fulfill this objective, comparisons between observations and model results are necessary. Knowledge of these model uncertainties is therefore necessary, although usually not considered, to estimate the ...
Gronoff, Guillaume +5 more
openaire +2 more sources
Simulation and analysis of radiant intensity for critical [PDF]
Atmospheric oxygen A-band (759-767nm) airglow has strong radiation intensity in the visible band, and the global atmospheric temperature field can be obtained based on the oxygen A-spectrum line.
Li Shaoze, Si Fuqi
doaj +1 more source

