We have performed ground-based airglow observations with a tilting filter spectrometer to determine ro-tational temperatures in the mesopause region since 1984. Although quite simple in principle, the success of the technique depends on a number of non-trivial details, including corrections for measurements under less favorable conditions, as, for instance, full moon nights. Successive improvements have finally led to nearly continuous observations, since August 1997, with more than 200 nights of useful data per year. The technique is described in some detail and recent results are discussed
The mesopause region (~90 km altitude) is the coldest region of our atmosphere, and is found at the ...
Spectroscopic measurements of the night airglow were taken at mid latitude over a period of four mon...
Abstract. Ground-based spectrographical observations of infrared emissions of the mesopause region h...
In this work we present a methodology to calculate the temperature in the upper mesosphere using a s...
The research studied the comparison of the night air temperatures and the atomic oxygen airglow inte...
Ground based measurements of the hydroxyl airglow started in Trondheim (63.4 N, 10.4 E) 20. November...
Spectra of the O2(a1 Δg) airglow emission band at 1.27 μm have been recorded during twilight at May...
The physics of the hydroxyl (OH) layer located in the Mesosphere and Lower Thermosphere (MLT) has be...
The Cariri Airglow Observatory has been in operation since November, 1997. This observatory has a mu...
Spectra of the O2(a1Δg) airglow emission band at 1.27 µm have been recorded during twilight a...
Astronomical spectroscopic observations from ground-based telescopes contain background emission lin...
Tropical airglow work during the last few years is reviewed. Airglow instrumentation is becoming mor...
At nighttime the strongest source of radiation is the hydroxyl night glow. By measuringthe different...
The airglow OH (8-3) and (6-2) band rotational temperatures were measured and compared using two sca...
The mesopause region (~90 km altitude) is the coldest region of our atmosphere, and is found at the ...
The mesopause region (~90 km altitude) is the coldest region of our atmosphere, and is found at the ...
Spectroscopic measurements of the night airglow were taken at mid latitude over a period of four mon...
Abstract. Ground-based spectrographical observations of infrared emissions of the mesopause region h...
In this work we present a methodology to calculate the temperature in the upper mesosphere using a s...
The research studied the comparison of the night air temperatures and the atomic oxygen airglow inte...
Ground based measurements of the hydroxyl airglow started in Trondheim (63.4 N, 10.4 E) 20. November...
Spectra of the O2(a1 Δg) airglow emission band at 1.27 μm have been recorded during twilight at May...
The physics of the hydroxyl (OH) layer located in the Mesosphere and Lower Thermosphere (MLT) has be...
The Cariri Airglow Observatory has been in operation since November, 1997. This observatory has a mu...
Spectra of the O2(a1Δg) airglow emission band at 1.27 µm have been recorded during twilight a...
Astronomical spectroscopic observations from ground-based telescopes contain background emission lin...
Tropical airglow work during the last few years is reviewed. Airglow instrumentation is becoming mor...
At nighttime the strongest source of radiation is the hydroxyl night glow. By measuringthe different...
The airglow OH (8-3) and (6-2) band rotational temperatures were measured and compared using two sca...
The mesopause region (~90 km altitude) is the coldest region of our atmosphere, and is found at the ...
The mesopause region (~90 km altitude) is the coldest region of our atmosphere, and is found at the ...
Spectroscopic measurements of the night airglow were taken at mid latitude over a period of four mon...
Abstract. Ground-based spectrographical observations of infrared emissions of the mesopause region h...