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1. Identity statement
Reference TypeJournal Article
Sitemtc-m16c.sid.inpe.br
Holder Codeisadg {BR SPINPE} ibi 8JMKD3MGPCW/3DT298S
Identifier8JMKD3MGP8W/349BH3P
Repositorysid.inpe.br/mtc-m18@80/2008/11.21.11.02
Last Update2008:11.21.11.02.30 (UTC) administrator
Metadata Repositorysid.inpe.br/mtc-m18@80/2008/11.21.11.02.32
Metadata Last Update2018:06.04.04.05.46 (UTC) administrator
Secondary KeyINPE--PRE/
ISSN0992-7689
Citation KeyRodriguesHysePaul:2008:LaWaBo
TitleCoherent backscatter radar imaging in Brazil: large-scale waves in the bottomside F-region at the onset of equatorial spread F
Year2008
Access Date2024, June 16
Secondary TypePRE PI
Number of Files1
Size2654 KiB
2. Context
Author1 Rodrigues, F. S.
2 Hysell, D. L.
3 Paula, Eurico Rodrigues de
Resume Identifier1
2
3 8JMKD3MGP5W/3C9JH2U
Group1
2
3 DAE-CEA-INPE-MCT-BR
Affiliation1 Cornell University, Earth and Atmospheric Sciences
2 Cornell University, Earth and Atmospheric Sciences
3 Instituto Nacional de Pesquisas Espaciais (INPE)
JournalAnnales Geophysicae
Volume26
Number11
Pages3355-3364
History (UTC)2008-11-21 11:02:33 :: simone -> banon ::
2009-07-14 21:35:18 :: banon -> administrator ::
2010-05-11 01:25:03 :: administrator -> banon ::
2010-05-11 15:20:59 :: banon -> administrator ::
2013-02-20 15:28:50 :: administrator -> marciana :: 2008
2013-03-07 13:33:46 :: marciana -> administrator :: 2008
2018-06-04 04:05:46 :: administrator -> marciana :: 2008
3. Content and structure
Is the master or a copy?is the master
Content Stagecompleted
Transferable1
Content TypeExternal Contribution
Version Typepublisher
AbstractThe 30 MHz coherent backscatter radar located at the equatorial observatory in São Luís, Brazil (2.59° S, 44.21° W, −2.35° dip lat) has been upgraded to perform coherent backscatter radar imaging. The wide field-of-view of this radar makes it well suited for radar imaging studies of ionospheric irregularities. Radar imaging observations were made in support to the spread F Experiment (SpreadFEx) campaign. This paper describes the system and imaging technique and presents results from a bottom-type layer that preceded fully-developed radar plumes on 25 October 2005. The radar imaging technique was able to resolve decakilometric structures within the bottom-type layer. These structures indicate the presence of large-scale waves (~35 km) in the bottomside F-region with phases that are alternately stable and unstable to wind-driven gradient drift instabilities. The observations suggest that these waves can also cause the initial perturbation necessary to initiate the Generalized Rayleigh-Taylor instability leading to spread F. The electrodynamic conditions and the scale length of the bottom-type layer structures suggest that the waves were generated by the collisional shear instability. These results indicate that monitoring bottom-type layers may provide helpful diagnostics for spread F forecasting.
AreaCEA
Arrangementurlib.net > BDMCI > Fonds > Produção anterior à 2021 > DIDAE > Coherent backscatter radar...
doc Directory Contentaccess
source Directory Contentthere are no files
agreement Directory Contentthere are no files
4. Conditions of access and use
data URLhttp://urlib.net/ibi/8JMKD3MGP8W/349BH3P
zipped data URLhttp://urlib.net/zip/8JMKD3MGP8W/349BH3P
Languageen
Target Filecoherent.pdf
User Groupadministrator
banon
marciana
simone
Visibilityshown
Archiving Policyallowpublisher allowfinaldraft
Read Permissionallow from all
Update Permissionnot transferred
5. Allied materials
Next Higher Units8JMKD3MGPCW/3ETL868
Citing Item Listsid.inpe.br/mtc-m21/2012/07.13.14.45.35 1
sid.inpe.br/bibdigital/2013/09.29.20.43 1
DisseminationWEBSCI; PORTALCAPES.
Host Collectionsid.inpe.br/mtc-m18@80/2008/03.17.15.17
6. Notes
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7. Description control
e-Mail (login)marciana
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