Model results of OH airglow considering four different wavelength regions to derive night-time atomic oxygen and atomic hydrogen in the mesopause region
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Published:2019-02-12
Issue:3
Volume:19
Page:1835-1851
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ISSN:1680-7324
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Container-title:Atmospheric Chemistry and Physics
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language:en
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Short-container-title:Atmos. Chem. Phys.
Author:
Fytterer Tilo, von Savigny Christian, Mlynczak Martin, Sinnhuber MiriamORCID
Abstract
Abstract. Based on the zero-dimensional box model Module Efficiently Calculating the Chemistry of the Atmosphere/Chemistry As
A Box model Application (CAABA/MECCA-3.72f), an OH
airglow model was developed to derive night-time number densities of atomic
oxygen ([O(3P)]) and atomic hydrogen ([H]) in the mesopause region
(∼75–100 km). The profiles of [O(3P)] and [H] were
calculated from OH airglow emissions measured at 2.0 µm by the Sounding of the Atmosphere using Broadband Emission Radiography (SABER)
instrument on board NASA's Thermosphere Ionosphere Mesosphere Energetics and Dynamics (TIMED)
satellite.
The two target species were used to initialize the OH airglow
model, which was empirically adjusted to fit four different OH airglow
emissions observed by the satellite/instrument configuration TIMED/SABER at
2.0 µm and at 1.6 µm as well as measurements by
the Scanning Imaging Absorption Spectrometer for Atmospheric Chartography (SCIAMACHY) instrument on board the Environmental Satellite (ENVISAT)
of the transitions OH(6-2)
and OH(3-1). Comparisons between
the “best-fit model” obtained here and the satellite measurements suggest
that deactivation of vibrationally excited OH(ν) via OH(ν≥7)+O2 might favour relaxation to OH(ν′≤5)+O2 by
multi-quantum quenching. It is further indicated that the deactivation
pathway to OH(ν′=ν-5)+O2 dominates. The results also provide
general support of the recently proposed mechanism OH(ν)+O(3P)→OH(0≤ν′≤ν-5)+O(1D) but suggest slower rates of
OH(ν=8,7,6,5)+O(3P), partly disagreeing with laboratory
experiments. Additionally, deactivation to OH(ν′=ν-5)+O(1D)
might be preferred. The profiles of [O(3P)] and [H] derived here are
plausible between 80 and 95 km but should be regarded as an upper limit.
The values of [O(3P)] obtained in this study agree with the
corresponding TIMED/SABER values between 80 and 85 km but are larger from
85 to 95 km due to different relaxation assumptions of OH(ν)+O(3P).
The [H] profile found here is generally larger than TIMED/SABER [H] by about
50 % from 80 to 95 km, which is primarily attributed to our faster OH(ν=8)+O2 rate.
Funder
Deutsche Forschungsgemeinschaft
Publisher
Copernicus GmbH
Subject
Atmospheric Science
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