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@ARTICLE{Funke:22367,
author = {Funke, B. and López-Puertas, M. and Garda-Comas, M. and
Kaufmann, M. and Stiller, G.P.},
title = {{GRANANDA}: {A} {G}eneric {RA}diative tra{N}sfer {A}n{D}
non-{LTE} population},
journal = {Journal of quantitative spectroscopy $\&$ radiative
transfer},
volume = {113},
issn = {0022-4073},
address = {New York, NY [u.a.]},
publisher = {Elsevier},
reportid = {PreJuSER-22367},
pages = {1771 - 1817},
year = {2012},
note = {We would like to acknowledge the enormous effort of Alain
Barbe, Claude Camy-Peiret, and Jean-Marie Flaud for
improving and supplying spectroscopic data that are crucial
for the non-LIE studies. We give special thanks to
Jean-Marie Flaud for providing the spectroscopic data for
many of the O<INF>3</INF> and NO<INF>2</INF> hot bands in
addition to those in HITRAN2008. We also thank F.J.
Martin-Torres for useful advices during the early
development of the algorithm, and Miguel A. Lopez-Valverde,
Sergio Gil-Lopez, Mariliza Koukouli and Diego
Bermejo-Pantaleon for useful comments and suggestions. The
IAA team was partially supported by the Spanish MCINN under
projects AYA2008-03498/ESP, AYA2011-23552, "ASTROMOL"
CSD2009-00038, and EC FEDER funds.},
abstract = {We present in this paper the Generic RAdiative traNsfer AnD
non-LTE population Algorithm (GRANADA). This model is able
to compute non-LIE populations for vibrational, rotational,
spin (i.e., NO and OH), and electronic (i.e., O-2) states in
a given planetary atmosphere. The model is very flexible and
can be used for computing very accurate non-LIE populations
or for calculating reasonably accurate but at high speed
non-LIE populations in order to implement it into non-LIE
remote sensing retrievals. We describe the model in detail
and present an update of the non-LIE collisional processes
and their rate coefficients for the most important molecules
in Earth's atmosphere. In addition, we have applied the
model to the most important atmospheric infrared emitters
including 13 species (H2O, CO2, O-3, N2O, CO, CH4, O-2, NO,
NO2, HNO3, OH, N-2, and HCN) and 460 excited vibrational or
electronic energy levels. Non-LIE populations for all these
energy levels have been calculated for 48 reference
atmospheres expanding from the surface up to 200 km,
including seasonal (January, April, July and October),
latitudinal (75 degrees S, 45 degrees S, 10 degrees S, 10
degrees N, 45 degrees N, 75 degrees N) and diurnal (day and
night) coverages. The effects of the most recent updates of
the non-LIE collisional parameters on the non-LIE
populations are briefly described. This climatology is
available online to the community and it can be used for
estimating non-LTE effects at specific conditions and for
testing and validation studies. (C) 2012 Elsevier Ltd. All
rights reserved.},
keywords = {J (WoSType)},
cin = {IEK-7},
ddc = {530},
cid = {I:(DE-Juel1)IEK-7-20101013},
pnm = {Atmosphäre und Klima},
pid = {G:(DE-Juel1)FUEK491},
shelfmark = {Spectroscopy},
typ = {PUB:(DE-HGF)16},
UT = {WOS:000306615400004},
doi = {10.1016/j.jqsrt.2012.05.001},
url = {https://juser.fz-juelich.de/record/22367},
}