Line emission from hydroxyl (OH) molecules at altitudes of about 90 km strongly contributes to the Earth's night-sky brightness and is therefore used as an important indicator of atmospheric chemistry and dynamics. However, interpreting the measurements can be ambiguous since necessary molecular parameters and the internal state of OH are not well known. Based on high-quality spectral data, we investigated these issues and found solutions for a better understanding of the OH line intensities
Rotational temperatures Trot from OH line intensities are an important approach to study the Earth's...
Nightglow within the mesopause region of the atmosphere is dominated by the infrared emissions from ...
Emissions from the OH Meinel bands are routinely used to determine rotational temperatures that are ...
Line emission from hydroxyl (OH) molecules at altitudes of about 90 km strongly contributes to the E...
Chemiluminescent radiation of the vibrationally and rotationally excited hydroxyl (OH) radical, whic...
Spectroscopic measurements of the hydroxyl (OH) airglow emissions are often used to infer neutral te...
The nocturnal mesopause region of the Earth's atmosphere radiates chemiluminescent emission from var...
Astronomical spectroscopic observations from ground-based telescopes contain background emission lin...
Satellite measurements from the Aura MLS instrument show a layer of OH near 82 km in the night. This...
The Earth's nighttime radiation in the range from the near-UV to the near-IR mainly originates betwe...
A number of different OH Meinel band excitation models are used to investigate the extent to which q...
Chemiluminescent radiation of the vibrationally and rotationally excited hydroxyl (OH) radical, whic...
The layer of vibrationally excited hydroxyl (OH*) near the mesopause in Earth's atmosphere is widely...
This brief note introduces several analytical approaches to OH* layer parameters. The number density...
Measurements of hydroxyl (OH*) airglow intensity are a straightforward and cost-efficient method whi...
Rotational temperatures Trot from OH line intensities are an important approach to study the Earth's...
Nightglow within the mesopause region of the atmosphere is dominated by the infrared emissions from ...
Emissions from the OH Meinel bands are routinely used to determine rotational temperatures that are ...
Line emission from hydroxyl (OH) molecules at altitudes of about 90 km strongly contributes to the E...
Chemiluminescent radiation of the vibrationally and rotationally excited hydroxyl (OH) radical, whic...
Spectroscopic measurements of the hydroxyl (OH) airglow emissions are often used to infer neutral te...
The nocturnal mesopause region of the Earth's atmosphere radiates chemiluminescent emission from var...
Astronomical spectroscopic observations from ground-based telescopes contain background emission lin...
Satellite measurements from the Aura MLS instrument show a layer of OH near 82 km in the night. This...
The Earth's nighttime radiation in the range from the near-UV to the near-IR mainly originates betwe...
A number of different OH Meinel band excitation models are used to investigate the extent to which q...
Chemiluminescent radiation of the vibrationally and rotationally excited hydroxyl (OH) radical, whic...
The layer of vibrationally excited hydroxyl (OH*) near the mesopause in Earth's atmosphere is widely...
This brief note introduces several analytical approaches to OH* layer parameters. The number density...
Measurements of hydroxyl (OH*) airglow intensity are a straightforward and cost-efficient method whi...
Rotational temperatures Trot from OH line intensities are an important approach to study the Earth's...
Nightglow within the mesopause region of the atmosphere is dominated by the infrared emissions from ...
Emissions from the OH Meinel bands are routinely used to determine rotational temperatures that are ...