This brief note introduces several analytical approaches to OH* layer parameters. The number density and height of the OH* layer peak are determined by the distributions of atomic oxygen and temperature, and by corresponding vertical gradients. The theory can be applied to satellite-borne and ground-based airglow measurements, as well as to model results
This work investigates the mesospheric OH* airglow layer. Ground-based observations of its Meinel em...
The physics of the hydroxyl (OH) layer located in the Mesosphere and Lower Thermosphere (MLT) has be...
Mesospheric OH radiance limb profiles measured by the Sounding of the Atmosphere using Broadband Emi...
This brief note introduces several analytical approaches to OH* layer parameters. The number de...
The layer of vibrationally excited hydroxyl (OH*) near the mesopause in Earth's atmosphere is widely...
Measurements of hydroxyl (OH*) airglow intensity are a straightforward and cost-efficient method whi...
Measurements of hydroxyl nightglow emissions over Longyearbyen (78 N, 16 E) recorded simultaneously...
Line emission from hydroxyl (OH) molecules at altitudes of about 90 km strongly contributes to the E...
Ground-based observations show a phase shift in semi-annual variation of excited hydroxyl (OH∗) emis...
Nightglow within the mesopause region of the atmosphere is dominated by the infrared emissions from ...
The mesospheric OH layer varies on several timescales, primarily driven by variations in atomic oxy...
Diurnal variations in hydroxyl (OH) in the stratosphere and mesosphere are analyzed using measuremen...
Measurements of hydroxyl nightglow emissions over Longyearbyen (78° N, 16° E) recorded simu...
Simultaneous measurements of mesospheric OH (6–2) Meinel and O2 (0–1) Atmospheric band emissions fro...
A provisional Atomic Oxygen Reference model was derived from average monthly ozone profiles and the ...
This work investigates the mesospheric OH* airglow layer. Ground-based observations of its Meinel em...
The physics of the hydroxyl (OH) layer located in the Mesosphere and Lower Thermosphere (MLT) has be...
Mesospheric OH radiance limb profiles measured by the Sounding of the Atmosphere using Broadband Emi...
This brief note introduces several analytical approaches to OH* layer parameters. The number de...
The layer of vibrationally excited hydroxyl (OH*) near the mesopause in Earth's atmosphere is widely...
Measurements of hydroxyl (OH*) airglow intensity are a straightforward and cost-efficient method whi...
Measurements of hydroxyl nightglow emissions over Longyearbyen (78 N, 16 E) recorded simultaneously...
Line emission from hydroxyl (OH) molecules at altitudes of about 90 km strongly contributes to the E...
Ground-based observations show a phase shift in semi-annual variation of excited hydroxyl (OH∗) emis...
Nightglow within the mesopause region of the atmosphere is dominated by the infrared emissions from ...
The mesospheric OH layer varies on several timescales, primarily driven by variations in atomic oxy...
Diurnal variations in hydroxyl (OH) in the stratosphere and mesosphere are analyzed using measuremen...
Measurements of hydroxyl nightglow emissions over Longyearbyen (78° N, 16° E) recorded simu...
Simultaneous measurements of mesospheric OH (6–2) Meinel and O2 (0–1) Atmospheric band emissions fro...
A provisional Atomic Oxygen Reference model was derived from average monthly ozone profiles and the ...
This work investigates the mesospheric OH* airglow layer. Ground-based observations of its Meinel em...
The physics of the hydroxyl (OH) layer located in the Mesosphere and Lower Thermosphere (MLT) has be...
Mesospheric OH radiance limb profiles measured by the Sounding of the Atmosphere using Broadband Emi...