OH level populations and accuracies of Einstein-<i>A</i> coefficients from hundreds of measured lines
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Published:2020-05-06
Issue:9
Volume:20
Page:5269-5292
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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:
Noll StefanORCID, Winkler HolgerORCID, Goussev Oleg, Proxauf Bastian
Abstract
Abstract. OH airglow is an important nocturnal emission of the Earth's mesopause region.
As it is chemiluminescent radiation in a thin medium, the population
distribution over the various roto-vibrational OH energy levels of the
electronic ground state is not in local thermodynamic equilibrium (LTE). In
order to better understand these non-LTE effects, we studied hundreds of OH
lines in a high-quality mean spectrum based on observations with the
high-resolution Ultraviolet and Visual Echelle Spectrograph at Cerro Paranal
in Chile. Our derived populations cover vibrational levels between v=3 and 9, rotational levels up to N=24, and individual Λ-doublet
components when resolved. As the reliability of these results critically
depends on the Einstein-A coefficients used, we tested six different sets and
found clear systematic errors in all of them, especially for Q-branch lines
and individual Λ-doublet components. In order to minimise the
deviations in the populations for the same upper level, we used the most
promising coefficients from Brooke et al. (2016) and further
improved them with an empirical correction approach. The resulting rotational
level populations show a clear bimodality for each v, which is characterised
by a probably fully thermalised cold component and a hot population where the
rotational temperature increases between v=9 and 4 from about 700 to about
7000 K, and the corresponding contribution to the total population at the
lowest N decreases by an order of magnitude. The presence of the hot
populations causes non-LTE contributions to rotational temperatures at low
N, which can be estimated quite robustly based on the two-temperature model.
The bimodality is also clearly indicated by the dependence of the populations
on changes in the effective emission height of the OH emission layer. The
degree of thermalisation decreases with increasing layer height due to a
higher fraction of the hot component. Our high-quality population data are
promising with respect to a better understanding of the OH thermalisation
process.
Publisher
Copernicus GmbH
Subject
Atmospheric Science
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