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1. Identity statement
Reference TypeJournal Article
Sitemtc-m21b.sid.inpe.br
Holder Codeisadg {BR SPINPE} ibi 8JMKD3MGPCW/3DT298S
Identifier8JMKD3MGP3W34P/3PJ5D6E
Repositorysid.inpe.br/mtc-m21b/2017/09.04.19.23
Last Update2017:09.04.19.23.11 (UTC) administrator
Metadata Repositorysid.inpe.br/mtc-m21b/2017/09.04.19.23.11
Metadata Last Update2018:06.04.02.27.48 (UTC) administrator
DOI10.1002/2017JA023942
ISSN2169-9402
Citation KeyHardingMaQiFiMaNoWr:2017:AtScEf
TitleAtmospheric scattering effects on ground-based measurements of thermospheric vertical wind, horizontal wind, and temperature
Year2017
MonthJuly
Access Date2024, Apr. 25
Type of Workjournal article
Secondary TypePRE PI
Number of Files1
Size1137 KiB
2. Context
Author1 Harding, Brian. J.
2 Makela, Jonathan J.
3 Qin, Jianqi
4 Fisher, Daniel J.
5 Martins, Carlos R.
6 Noto, John
7 Wrasse, Cristiano Max
Group1
2
3
4
5
6
7 DIDAE-CGCEA-INPE-MCTIC-GOV-BR
Affiliation1 University of Illinois at Urbana-Champaign
2 University of Illinois at Urbana-Champaign
3 University of Illinois at Urbana-Champaign
4 University of Illinois at Urbana-Champaign
5 Boston University
6 Computational Physics, Inc
7 Instituto Nacional de Pesquisas Espaciais (INPE)
Author e-Mail Address1
2
3
4
5
6
7 cristiano.wrasse@inpe.br
JournalJournal of Geophysical Research: Space Physics
Volume122
Number7
Pages7654-7669
History (UTC)2017-09-04 19:23:11 :: simone -> administrator ::
2017-09-04 19:23:12 :: administrator -> simone :: 2017
2017-09-04 19:25:53 :: simone -> administrator :: 2017
2018-06-04 02:27:48 :: administrator -> simone :: 2017
3. Content and structure
Is the master or a copy?is the master
Content Stagecompleted
Transferable1
Content TypeExternal Contribution
Version Typepublisher
AbstractGround-based Fabry-Perot interferometers routinely observe large vertical winds in the thermosphere, sometimes reaching over 100m/s. These observations, which use the Doppler shift of the 630.0nm airglow emission to estimate the wind, have long been at odds with theory. We present a summary of 5years of data from the North American Thermosphere-Ionosphere Observing Network, showing that large apparent vertical winds are a persistent feature at midlatitudes during geomagnetic storms. We develop a radiative transfer model which demonstrates that these measurements can be explained as an artifact of the scattering of light in the troposphere. In addition to the example from midlatitudes, we apply the model to low latitudes, where we show that the postsunset vertical winds routinely measured over Brazil are explained in part by atmospheric scattering. Measurements of the horizontal wind and temperature are also affected, with errors reaching 400m/s and 200K in the most extreme cases.
AreaCEA
Arrangementurlib.net > BDMCI > Fonds > Produção anterior à 2021 > DIDAE > Atmospheric scattering effects...
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4. Conditions of access and use
data URLhttp://urlib.net/ibi/8JMKD3MGP3W34P/3PJ5D6E
zipped data URLhttp://urlib.net/zip/8JMKD3MGP3W34P/3PJ5D6E
Languageen
Target Fileharding_atmospheric.pdf
User Groupsimone
Reader Groupadministrator
simone
Visibilityshown
Archiving Policydenypublisher6 allowfinaldraft
Read Permissionallow from all
Update Permissionnot transferred
5. Allied materials
Next Higher Units8JMKD3MGPCW/3ETL868
DisseminationWEBSCI; AGU; MGA; COMPENDEX.
Host Collectionsid.inpe.br/mtc-m21b/2013/09.26.14.25.20
6. Notes
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