% IMPORTANT: The following is UTF-8 encoded. This means that in the presence
% of non-ASCII characters, it will not work with BibTeX 0.99 or older.
% Instead, you should use an up-to-date BibTeX implementation like “bibtex8” or
% “biber”.
@ARTICLE{Song:841897,
author = {Song, Rui and Kaufmann, Martin and Ern, Manfred and Liu,
Guang and Riese, Martin and Ungermann, Jörn},
title = {{T}omographic reconstruction of atmospheric gravity wave
parameters from airglow observations},
journal = {Atmospheric measurement techniques},
volume = {10},
number = {12},
issn = {1867-8548},
address = {Katlenburg-Lindau},
publisher = {Copernicus},
reportid = {FZJ-2018-00194},
pages = {4601 - 4612},
year = {2017},
abstract = {Gravity waves (GWs) play an important role in the dynamics
of the mesosphere and lower thermosphere (MLT). Therefore,
global observations of GWs in the MLT region are of
particular interest. The small scales of GWs, however, pose
a major problem for the observation of GWs from space. We
propose a new observation strategy for GWs in the mesopause
region by combining limb and sub-limb satellite-borne remote
sensing measurements for improving the spatial resolution of
temperatures that are retrieved from atmospheric soundings.
In our study, we simulate satellite observations of the
rotational structure of the O2 A-band nightglow. A key
element of the new method is the ability of the instrument
or the satellite to operate in so-called "target mode", i.e.
to point at a particular point in the atmosphere and collect
radiances at different viewing angles. These multi-angle
measurements of a selected region allow for tomographic 2-D
reconstruction of the atmospheric state, in particular of GW
structures. The feasibility of this tomographic retrieval
approach is assessed using simulated measurements. It shows
that one major advantage of this observation strategy is
that GWs can be observed on a much smaller scale than
conventional observations. We derive a GW sensitivity
function, and it is shown that "target mode" observations
are able to capture GWs with horizontal wavelengths as short
as ∼ 50 km for a large range of vertical
wavelengths. This is far better than the horizontal
wavelength limit of 100–200 km obtained from
conventional limb sounding.},
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) / HITEC - Helmholtz
Interdisciplinary Doctoral Training in Energy and Climate
Research (HITEC) (HITEC-20170406)},
pid = {G:(DE-HGF)POF3-244 / G:(DE-Juel1)HITEC-20170406},
typ = {PUB:(DE-HGF)16},
UT = {WOS:000416551700002},
doi = {10.5194/amt-10-4601-2017},
url = {https://juser.fz-juelich.de/record/841897},
}