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@ARTICLE{Bracher:41265,
author = {Bracher, A. and Bovensmann, H. and Bramsted, K. and
Burrows, J. P. and von Clarmann, T. and Eichmann, K.-U. and
Fischer, H. and Funke, B. and Gil-Lopez, S. and Glatthor, G.
P. and Grabowski, U. and Höpfner, M. and Kaufmann, M. and
Kellmann, S. and Kiefer, M. and Koukouli, M. E. and Linden,
A. and Lopez-Puertas, M. L. and Mengistu-Tsidu, G. and Milz,
M. and Noel, S. and Rohen, G. and Rozanov, A. and Rozanov,
V. V. and von Savigny, C. and Sinnhuber, M. and Skupin, J.
and Steck, T. and Stiller, G. P. and Wang, D.-Y. and Weber,
M. and Wuttke, M. W.},
title = {{C}ross comparison of {O}3 and {NO}2 measured by the
atmospheric {ENVISAT} instruments {GOMOS}, {MIPAS}, and
{SCIAMACHY}},
journal = {Advances in space research},
volume = {36},
issn = {0273-1177},
address = {Amsterdam [u.a.]},
publisher = {Elsevier Science},
reportid = {PreJuSER-41265},
pages = {855 - 867},
year = {2005},
note = {Record converted from VDB: 12.11.2012},
abstract = {Vertical profiles Of O-3 and NO2 abundances from the
atmospheric instruments GOMOS (Global Ozone Monitoring by
the Occultation of Stars), MIPAS (Michelson Interferometer
for Passive Atmospheric Sounding) and SCIAMACHY (Scanning
Imaging Spectrometer for Atmospheric Chartography) all
on-board the recently launched European Space Agency (ESA)
Environmental Satellite (ENVISAT) are intercompared. These
comparisons contribute to the validation of these data
products by detecting systematic deviations, for example,
wrong tangent height determinations, spectroscopic errors,
and others. The cross comparison includes GOMOS data
products retrieved by the GOMOS prototype processor from
ACRI (Sophia Antipolis, France), the scientific SCIAMACHY
data products from the Institute of Environmental Physics at
University of Bremen (IUP) and the scientific MIPAS data
products from the Institute for Meteorology and Climate
Research in Karlsruhe (IMK) and Institute of Astrophysics in
Andalusia (IAA). Coincident measurements were identified by
limiting the time difference to 100 min (duration of one
orbit) and less than 500 km between two observation points.
When lower stratospheric ozone is strongly depleted during
polar spring, a homogeneity condition was further imposed on
the satellite measurements by requiring an upper limit on
the potential vorticity difference at the 475 K isentrope
between both observations. Since geographically coincident
NO2 measurements of the three instruments are performed
during different times of the day and NO2 has a rather
strong diurnal variability, matches of NO2 profiles were
compared only where the solar zenith angle difference was
below 5 degrees. First results of the cross comparison show
an agreement within $15\%$ between 21 and 40 km altitude for
O-3 profiles and an agreement within $20\%$ between 27 and
40 km altitude for NO2 profiles among the GOMOS, MIPAS and
SCIAMACHY measurements. (c) 2005 COSPAR. Published by
Elsevier Ltd. All rights reserved.},
keywords = {S (WoSType)},
cin = {ICG-I},
ddc = {520},
cid = {I:(DE-Juel1)VDB47},
pnm = {Chemie und Dynamik der Geo-Biosphäre},
pid = {G:(DE-Juel1)FUEK257},
shelfmark = {Engineering, Aerospace / Astronomy $\&$ Astrophysics /
Geosciences, Multidisciplinary / Meteorology $\&$
Atmospheric Sciences},
typ = {PUB:(DE-HGF)16},
UT = {WOS:000235478400012},
doi = {10.1016/j.asr.2005.04.005},
url = {https://juser.fz-juelich.de/record/41265},
}