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@ARTICLE{Zhu:856720,
author = {Zhu, Yajun and Kaufmann, Martin},
title = {{A}tomic {O}xygen {A}bundance {R}etrieved {F}rom
{SCIAMACHY} {H}ydroxyl {N}ightglow {M}easurements},
journal = {Geophysical research letters},
volume = {45},
number = {17},
issn = {0094-8276},
address = {Hoboken, NJ},
publisher = {Wiley},
reportid = {FZJ-2018-06071},
pages = {9314 - 9322},
year = {2018},
abstract = {We present a new atomic oxygen data set based on Scanning
Imaging Absorption Spectrometer for Atmospheric CHartographY
(SCIAMACHY) hydroxyl short‐wave infrared data. The OH
spectra stem from the OH(9‐6) ro‐vibrational transition.
These data and atomic oxygen obtained from SCIAMACHY O(1S)
green line measurements, which is an independent data set in
terms of methodology and radiometry, typically agree within
$10–20\%.$ This confirms the corresponding models of OH
and O(1S), in particular, the relevance of the reaction
between atomic oxygen and ozone in the photochemical model.
The agreement between the SCIAMACHY data and the most recent
Sounding of the Atmosphere using Broadband Emission
Radiometry (SABER) atomic oxygen data set of Mlynczak et al.
(2018, https://doi.org/10.1029/2018GL077377) is
significantly better than for the previous SABER data set of
Mlynczak et al. (2013, https://doi.org/10.1002/jgrd.50401).
The agreement decreases if the SCIAMACHY forward model
parameters are applied to SABER data. A similar agreement is
achieved with the data of Panka et al. (2018,
https://doi.org/10.1029/2018GL077677), which was retrieved
from SABER data using a principally different retrieval
approach.},
cin = {IEK-7},
ddc = {550},
cid = {I:(DE-Juel1)IEK-7-20101013},
pnm = {244 - Composition and dynamics of the upper troposphere and
middle atmosphere (POF3-244)},
pid = {G:(DE-HGF)POF3-244},
typ = {PUB:(DE-HGF)16},
UT = {WOS:000445727500068},
doi = {10.1029/2018GL079259},
url = {https://juser.fz-juelich.de/record/856720},
}