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1. Identity statement
Reference TypeJournal Article
Sitemtc-m21d.sid.inpe.br
Holder Codeisadg {BR SPINPE} ibi 8JMKD3MGPCW/3DT298S
Identifier8JMKD3MGP3W34T/4835MGP
Repositorysid.inpe.br/mtc-m21d/2022/11.18.12.26
Last Update2022:11.18.12.26.26 (UTC) simone
Metadata Repositorysid.inpe.br/mtc-m21d/2022/11.18.12.26.26
Metadata Last Update2023:01.03.16.46.24 (UTC) administrator
DOI10.1186/s40623-022-01718-y
ISSN1880-5981
Citation KeyArrasResKepSenWic:2022:SpLaCh
TitleSporadic E layer characteristics at equatorial latitudes as observed by GNSS radio occultation measurements
Year2022
MonthNov.
Access Date2024, May 14
Type of Workjournal article
Secondary TypePRE PI
Number of Files1
Size2606 KiB
2. Context
Author1 Arras, Christina
2 Resende, Laysa Cristina Araújo
3 Kepkar, Ankur
4 Senevirathna, Gethmini
5 Wickert, Jens
ORCID1 0000-0002-2789-1005
Group1
2 DICEP-CGCE-INPE-MCTI-GOV-BR
Affiliation1 GFZ German Research Centre for Geosciences
2 Instituto Nacional de Pesquisas Espaciais (INPE)
3 GFZ German Research Centre for Geosciences
4 TU Berlin
5 GFZ German Research Centre for Geosciences
Author e-Mail Address1
2 laysa.resende@gmail.com
JournalEarth Planets and Space
Volume74
Number1
Pagese163
History (UTC)2022-11-18 12:26:26 :: simone -> administrator ::
2022-11-18 12:26:27 :: administrator -> simone :: 2022
2022-11-18 12:27:31 :: simone -> administrator :: 2022
2023-01-03 16:46:24 :: administrator -> simone :: 2022
3. Content and structure
Is the master or a copy?is the master
Content Stagecompleted
Transferable1
Content TypeExternal Contribution
Version Typepublisher
KeywordsGNSS radio occultation
Sporadic E layers
Equatorial ionosphere
AbstractScintillations in the signal-to-noise (SNR) profiles of GNSS radio occultation (RO) measurements at lower ionospheric altitudes are caused by compact layers of high ionization also known as sporadic E (Es) layers. It is widely accepted that Es layers are formed by the wind shear mechanism at northern and southern midlatitudes. However, approaching the equatorial regions, electric fields also control the formation and dispersal of these layers. In this paper we concentrate, in particular, on the occurrence rate and on the altitudes of Es layers appearing in a narrow band along the Earth's magnetic equator. We analyzed several million of RO profiles concerning sporadic E occurrence as well as altitude and observed a high daily, seasonal and longitudinal variability which is controlled partly by zonal winds and electric fields. Especially Es layers at higher altitudes show a clear anticorrelation with the zonal electric field intensity measured by the Swarm satellites. Further, we solve the existing contradiction of Es layer signatures being present in equatorial ionosonde measurements while they are only rarely seen in RO recordings.
AreaCEA
Arrangementurlib.net > BDMCI > Fonds > Produção a partir de 2021 > CGCE > Sporadic E layer...
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4. Conditions of access and use
data URLhttp://mtc-m21d.sid.inpe.br/ibi/8JMKD3MGP3W34T/4835MGP
zipped data URLhttp://mtc-m21d.sid.inpe.br/zip/8JMKD3MGP3W34T/4835MGP
Languageen
Target Files40623-022-01718-y.pdf
User Groupsimone
Reader Groupadministrator
simone
Visibilityshown
Archiving Policyallowpublisher allowfinaldraft
Update Permissionnot transferred
5. Allied materials
Next Higher Units8JMKD3MGPCW/46KTFK8
Citing Item Listsid.inpe.br/bibdigital/2022/04.03.17.52 1
DisseminationWEBSCI; PORTALCAPES; SCOPUS.
Host Collectionurlib.net/www/2021/06.04.03.40
6. Notes
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