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1. Identity statement
Reference TypeJournal Article
Sitemtc-m21b.sid.inpe.br
Holder Codeisadg {BR SPINPE} ibi 8JMKD3MGPCW/3DT298S
Identifier8JMKD3MGP3W34P/3NU3DHL
Repositorysid.inpe.br/mtc-m21b/2017/05.22.18.57
Last Update2017:05.22.18.57.54 (UTC) simone
Metadata Repositorysid.inpe.br/mtc-m21b/2017/05.22.18.57.54
Metadata Last Update2021:02.06.15.39.10 (UTC) administrator
DOI10.1002/2016JA023638
ISSN2169-9402
Citation KeyAndrioliBaXuYaChZh:2017:StTeGr
TitleStrong temperature gradients and vertical wind shear on MLT region associated to instability source at 23°S
Year2017
MonthApr.
Access Date2024, May 23
Type of Workjournal article
Secondary TypePRE PI
Number of Files1
Size1867 KiB
2. Context
Author1 Andrioli, Vânia Fátima
2 Batista, Paulo Prado
3 Xu, Jiyao
4 Yang, Guotao
5 Chi, Wang
6 Zhengkuan, Liu
Resume Identifier1
2 8JMKD3MGP5W/3C9JJ3H
Group1 CGCEA-CGCEA-INPE-MCTIC-GOV-BR
Affiliation1 Instituto Nacional de Pesquisas Espaciais (INPE)
2 Instituto Nacional de Pesquisas Espaciais (INPE)
3 Chinese Academy of Sciences
4 Chinese Academy of Sciences
5 Chinese Academy of Sciences
6 Chinese Academy of Sciences
Author e-Mail Address1 vania.andrioli@inpe.br
2 paulo.batista@inpe.br
JournalJournal of Geophysical Research: Space Physics
Volume122
Number4
Pages4500-4511
History (UTC)2017-05-22 18:57:54 :: simone -> administrator ::
2017-05-22 18:57:55 :: administrator -> simone :: 2017
2017-05-22 18:58:38 :: simone -> administrator :: 2017
2017-07-04 11:46:47 :: administrator -> simone :: 2017
2017-12-14 14:58:47 :: simone -> administrator :: 2017
2018-01-09 11:41:15 :: administrator -> simone :: 2017
2018-01-09 17:38:10 :: simone -> administrator :: 2017
2021-02-06 15:39:10 :: administrator -> simone :: 2017
3. Content and structure
Is the master or a copy?is the master
Content Stagecompleted
Transferable1
Content TypeExternal Contribution
Version Typepublisher
Keywordsconvective instability
dynamical instability
mesopause instabilities
meteor radar wind
Na lidar temperature
AbstractNa lidar temperature measurements were taken successfully from 2007 to 2009 in the mesopause region over São José dos Campos (23.1°S, 45.9°W). Strong gradients on these vertical temperature profiles are often observed. A simple theoretical study has shown that temperature gradient of at least −8 K/km is required concurrently with the typical tidal wind shear in order to generate dynamical instability in the MLT region. We have studied vertical shear in horizontal wind related to atmospheric tides, inferred by meteor radar, with the aim of analyzing instability occurrence. These wind measurements were taken from an all-sky meteor radar at Cachoeira Paulista (22.7°S, 45°W). Two years of simultaneous data, wind and temperature, were used in this analysis which represent 79 days, totalizing 589 h of simultaneous observations. We realize that the condition for the local Richardson number (Ri) dropping below the critical value of instability (Ri < 0.25) is often reached in 98% of the analyzed cases. The mean probabilities for occurrence of convective and dynamical instabilities, in the altitude region between 82 and 98 km, were observed to be about 3% and 17.5%, respectively. Additionally, vertical distribution of these probabilities has revealed a weak occurrence of dynamical instability around 90 km, and this fact can be related to the double mesopause typically observed in this site.
AreaCEA
Arrangementurlib.net > BDMCI > Fonds > Produção anterior à 2021 > CGCEA > Strong temperature gradients...
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4. Conditions of access and use
data URLhttp://urlib.net/ibi/8JMKD3MGP3W34P/3NU3DHL
zipped data URLhttp://urlib.net/zip/8JMKD3MGP3W34P/3NU3DHL
Languageen
Target Fileandrioli_strong.pdf
User Groupsimone
Reader Groupadministrator
simone
Visibilityshown
Archiving Policydenypublisher6 allowfinaldraft
Read Permissionallow from all
Update Permissionnot transferred
5. Allied materials
Next Higher Units8JMKD3MGPCW/3EU2FR5
Citing Item Listsid.inpe.br/bibdigital/2013/10.01.23.29 2
sid.inpe.br/mtc-m21/2012/07.13.14.58 1
DisseminationWEBSCI; AGU; MGA; COMPENDEX.
Host Collectionsid.inpe.br/mtc-m21b/2013/09.26.14.25.20
6. Notes
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