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1. Identity statement
Reference TypeJournal Article
Sitemtc-m16.sid.inpe.br
Holder Codeisadg {BR SPINPE} ibi 8JMKD3MGPCW/3DT298S
Identifier6qtX3pFwXQZsFDuKxG/EodUr
Repositorysid.inpe.br/marciana/2004/12.06.14.24
Last Update2004:12.06.02.00.00 (UTC) marciana
Metadata Repositorysid.inpe.br/marciana/2004/12.06.14.24.27
Metadata Last Update2024:05.13.16.19.38 (UTC) marciana
Secondary KeyINPE-11754-PRE/7113
ISSN0992-7689
Labelself-archiving-INPE-MCTIC-GOV-BR
Citation KeySahaiFBACPIAPB:2004:LoDiOb
TitleLongitudinal differences observed in the ionospheric F-region during the major geomagnetic storm of 31 March 2001
ProjectDinâmica de termosfera e ionosfera usando simulação computacional e medidas experimentais
Year2004
Access Date2024, May 16
Secondary TypePRE PI
Number of Files1
Size1803 KiB
2. Context
Author 1 Sahai, Y.
 2 Fagundes, P. R.
 3 Becker Guedes, F.
 4 Abalde, José Ricardo
 5 Crowley, G.
 6 Pi, X.
 7 Igarashi, K.
 8 Amarante, G. M.
 9 Pimenta, Alexandre Alvares
10 Bittencourt, José Augusto
Resume Identifier 1
 2
 3
 4
 5
 6
 7
 8
 9 8JMKD3MGP5W/3C9JGGL
10 8JMKD3MGP5W/3C9JHG7
Group 1
 2
 3
 4
 5
 6
 7
 8
 9 DAE-INPE-MCT-BR
10 DAE-INPE-MCT-BR
Affiliation 1 Universidade do Vale do Paraíba (UNIVAP)
 2 Universidade do Vale do Paraíba (UNIVAP)
 3 Universidade do Vale do Paraíba (UNIVAP)
 4 Universidade do Vale do Paraíba (UNIVAP)
 5 Southwest Research Institute
 6 Jet Propulsion Laboratory
 7 Communications Research Laboratory
 8 The Abdus Salam (ICTP)
 9 Instituto Nacional de Pesquisas Espaciais, Divisão de Aeronomia (INPE.DAE)
10 Instituto Nacional de Pesquisas Espaciais, Divisão de Aeronomia (INPE.DAE)
JournalAnnales Geophysicae
Volume22
Number9
Pages3221-3229
History (UTC)2004-12-14 12:53:57 :: sergio -> administrator ::
2006-09-28 22:28:05 :: administrator -> sergio ::
2008-01-07 12:53:38 :: sergio -> marciana ::
2008-04-04 18:55:55 :: marciana -> administrator ::
2008-06-10 22:28:04 :: administrator -> banon ::
2010-05-11 15:20:34 :: banon -> administrator ::
2012-10-20 15:14:27 :: administrator -> marciana :: 2004
2013-03-07 14:22:23 :: marciana -> administrator :: 2004
2018-06-05 01:21:09 :: administrator -> marciana :: 2004
3. Content and structure
Is the master or a copy?is the master
Content Stagecompleted
Transferable1
Content TypeExternal Contribution
Version Typepublisher
KeywordsAERONOMY
Ionosphere
Ionospheric disturbances
Modelling and forecasting
Magnetospheric physics
Storms and substorms
Atmospheric
Gravity waves
Equatorial ionosphere
Imaging observations
Plasma depletions
Mangetic storms
Wags campaign
Disturbances
AERONOMIA
Ionosfera
Distúrbios ionosféricos
Física magnetosférica
Tempestades
Ondas da gravidade atmosférica
Ionosfera equatorial
Observação de imagens
Tempestades magnéticas
AbstractA new ionospheric sounding station using a Canadian Advanced Digital Ionosonde (CADI) was established for routine measurements by the "Universidade do Vale do Paraiba (UNIVAP)" at Sao Jose dos Campos (23.2degrees S, 45.9degrees W), Brazil, in August 2000. A major geomagnetic storm with gradual commencement at about 01:00 UT was observed or 31 March 2001. In this paper, we present and discuss salient features from the ionospheric sounding measurements carried out at S. J. Campos on the three consecutive UT days 30 March (quiet), 31 March (disturbed) and I April (recovery) 2001. During most of the storm period. the foF2 values showed negative phase, whereas during the two storm-time peaks, large F-region height variations were observed. In order to study the longitudinal differences observed in the F-realon during the storm, the simultaneous ionospheric sounding measurements carried out at S. J. Campos. El Arenosillo (37.1degrees N, 6.7degrees W), Spain, Okinawa (26.3degrees N, 127.8degrees E), Japan and Wakkanai (45.5degrees N, 141.7degrees E), Japan, during the period 30 March-1 April 2001, have been analyzed. A comparison of the observed ionospheric parameters (h'F and foF2) in the two longitudinal zones (1. Japanese and 2. Brazilian-Spanish) shows both similarities and differences associated with the geomagnetic disturbances. Some latitudinal differences are also observed in the two longitudinal zones. In addition, global ionospheric TEC maps from the worldwide network of GPS receivers are presented, showing widespread TEC changes during both the main and recovery phases of the storm. The ionospheric sounding measurements are compared with the ASPEN-TIMEGCM model runs appropriate for the storm conditions. The model results produce better agreement during the quiet period. During the disturbed period, some of the observed F-region height variations are well reproduced by the model results. The model foF2 and TEC results differ considerably during the recovery period and indicate much stronger negative phase at all the stations, particularly at the low-latitude ones.
AreaCEA
Arrangementurlib.net > BDMCI > Fonds > Produção anterior à 2021 > DIDAE > Longitudinal differences observed...
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/6qtX3pFwXQZsFDuKxG/EodUr
zipped data URLhttp://urlib.net/zip/6qtX3pFwXQZsFDuKxG/EodUr
Languageen
Target Filelongitudinal differences.pdf
User Groupadministrator
banon
marciana
sergio
Visibilityshown
Copy HolderSID/SCD
Archiving Policyallowpublisher allowfinaldraft
Read Permissionallow from all
Update Permissionnot transferred
5. Allied materials
Next Higher Units8JMKD3MGPCW/3ETL868
Citing Item Listsid.inpe.br/bibdigital/2013/09.29.20.43 1
sid.inpe.br/mtc-m21/2012/07.13.14.51.32 1
DisseminationWEBSCI; PORTALCAPES; MGA; COMPENDEX.
Host Collectionsid.inpe.br/banon/2003/08.15.17.40
6. Notes
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