1. Identity statement | |
Reference Type | Journal Article |
Site | mtc-m21d.sid.inpe.br |
Holder Code | isadg {BR SPINPE} ibi 8JMKD3MGPCW/3DT298S |
Identifier | 8JMKD3MGP3W34T/47TD348 |
Repository | sid.inpe.br/mtc-m21d/2022/11.01.17.34 |
Last Update | 2022:11.01.17.34.43 (UTC) simone |
Metadata Repository | sid.inpe.br/mtc-m21d/2022/11.01.17.34.43 |
Metadata Last Update | 2023:01.23.17.06.34 (UTC) administrator |
DOI | 10.3390/atmos13101714 |
ISSN | 2073-4433 |
Citation Key | ResendeZADCMSCSAMC:2022:AnSpLa |
Title | Analysis of the Sporadic-E Layer Behavior in Different American Stations during the Days around the September 2017 Geomagnetic Storm |
Year | 2022 |
Month | Oct. |
Access Date | 2024, May 14 |
Type of Work | journal article |
Secondary Type | PRE PI |
Number of Files | 1 |
Size | 4625 KiB |
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2. Context | |
Author | 1 Resende, Laysa Cristina Araújo 2 Zhu, Yajun 3 Arras, Christina 4 Denardini, Clezio Marcos 5 Chen, Sony Su 6 Moro, Juliano 7 Silva, Diego Barros 8 Chagas, Ronan Arraes Jardim 9 Silva, Lígia Alves da 10 Andrioli, Vania Fátima 11 Marchezi, José Paulo 12 Carrasco, Alexander José |
ORCID | 1 2 3 4 0000-0002-3624-2461 5 0000-0001-6307-7484 6 7 8 9 10 0000-0001-9065-2122 11 0000-0002-2904-6411 |
Group | 1 DICEP-CGCE-INPE-MCTI-GOV-BR 2 3 4 DICEP-CGCE-INPE-MCTI-GOV-BR 5 GESAST-CEA-DIPGR-INPE-MCTI-GOV-BR 6 COESU-CGGO-INPE-MCTI-GOV-BR 7 YYY-CGCE-INPE-MCTI-GOV-BR 8 DISEP-CGCE-INPE-MCTI-GOV-BR 9 DIHPA-CGCE-INPE-MCTI-GOV-BR 10 DIHPA-CGCE-INPE-MCTI-GOV-BR 11 DICEP-CGCE-INPE-MCTI-GOV-BR 12 DICEP-CGCE-INPE-MCTI-GOV-BR |
Affiliation | 1 Instituto Nacional de Pesquisas Espaciais (INPE) 2 State Key Laboratory of Space Weather (NSSC) 3 German Research Centre for Geosciences (GFZ) 4 Instituto Nacional de Pesquisas Espaciais (INPE) 5 Instituto Nacional de Pesquisas Espaciais (INPE) 6 Instituto Nacional de Pesquisas Espaciais (INPE) 7 Instituto Nacional de Pesquisas Espaciais (INPE) 8 Instituto Nacional de Pesquisas Espaciais (INPE) 9 Instituto Nacional de Pesquisas Espaciais (INPE) 10 Instituto Nacional de Pesquisas Espaciais (INPE) 11 Instituto Nacional de Pesquisas Espaciais (INPE) 12 Instituto Nacional de Pesquisas Espaciais (INPE) |
Author e-Mail Address | 1 laysa.resende@inpe.br 2 3 4 clezio.denardin@inpe.br 5 sony.chen@inpe.br 6 julianopmoro@gmail.com 7 bar_diego@hotmail.com 8 ronan.arraes@inpe.br 9 ligia.alves01@gmail.com 10 vaniafatima@gmail.com 11 jpmarchezi@gmail.com 12 layerf2@gmail.com |
Journal | Atmosphere |
Volume | 13 |
Number | 10 |
Pages | e1714 |
Secondary Mark | B3_ENGENHARIAS_III B3_ENGENHARIAS_I B3_CIÊNCIAS_AMBIENTAIS B4_ENGENHARIAS_II B5_GEOCIÊNCIAS |
History (UTC) | 2022-11-01 17:34:43 :: simone -> administrator :: 2022-11-01 17:34:44 :: administrator -> simone :: 2022 2022-11-01 17:36:16 :: simone -> administrator :: 2022 2022-11-10 03:17:05 :: administrator -> simone :: 2022 2022-12-19 19:01:40 :: simone -> administrator :: 2022 2023-01-23 17:06:34 :: administrator -> simone :: 2022 |
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3. Content and structure | |
Is the master or a copy? | is the master |
Content Stage | completed |
Transferable | 1 |
Content Type | External Contribution |
Version Type | publisher |
Keywords | geomagnetic storm sporadic-E (Es) layer tidal winds |
Abstract | The development of sporadic-E (Es) layers over five Digisonde stations in the American sector is analyzed. This work aims to investigate the dynamic of such layers during the days around the geomagnetic storm that occurred on 8 September 2017. Therefore, a numerical model (MIRE) and Radio Occultation (RO) technique are used to analyze the E layer dynamics. The results show a downward movement in low-middle latitudes due to the wind components that had no significant changes before, during, and after the geomagnetic storm. In fact, our data and simulations showed weak Es layers over Boulder, Cachoeira Paulista, and Santa Maria, even though the winds were not low. However, the RO data show the terdiurnal and quarterdiurnal influence in the Es layer formation, which can explain this behavior. In addition, we observed an atypical Es layer type, slant Es layer (Ess), during the main phase of the magnetic storm over Boulder. The possible cause of the Ess layers was gravity waves. Another interesting point is the spreading Es layer occurrence associated with the KelvinHelmholtz Instability (KHI). Finally, it is confirmed that the disturbed electric field only influenced the Es layer dynamics in regions near the magnetic equator. |
Area | CEA |
Arrangement 1 | urlib.net > BDMCI > Fonds > Produção pgr ATUAIS > GES > Analysis of the... |
Arrangement 2 | urlib.net > BDMCI > Fonds > Produção a partir de 2021 > CGCE > Analysis of the... |
Arrangement 3 | urlib.net > BDMCI > Fonds > Produção a partir de 2021 > CGGO > Analysis of the... |
doc Directory Content | access |
source Directory Content | there are no files |
agreement Directory Content | |
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4. Conditions of access and use | |
data URL | http://mtc-m21d.sid.inpe.br/ibi/8JMKD3MGP3W34T/47TD348 |
zipped data URL | http://mtc-m21d.sid.inpe.br/zip/8JMKD3MGP3W34T/47TD348 |
Language | en |
Target File | atmosphere-13-01714-v2.pdf |
User Group | simone |
Reader Group | administrator simone |
Visibility | shown |
Archiving Policy | allowpublisher allowfinaldraft |
Update Permission | not transferred |
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5. Allied materials | |
Next Higher Units | 8JMKD3MGPCW/3F2PBEE 8JMKD3MGPCW/46KTFK8 8JMKD3MGPCW/46KUBT5 |
Citing Item List | sid.inpe.br/bibdigital/2022/04.03.22.35 6 sid.inpe.br/bibdigital/2022/04.03.17.52 1 |
Dissemination | WEBSCI; PORTALCAPES; SCOPUS. |
Host Collection | urlib.net/www/2021/06.04.03.40 |
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6. Notes | |
Empty Fields | alternatejournal archivist callnumber copyholder copyright creatorhistory descriptionlevel e-mailaddress format isbn label lineage mark mirrorrepository nextedition notes parameterlist parentrepositories previousedition previouslowerunit progress project readpermission resumeid rightsholder schedulinginformation secondarydate secondarykey session shorttitle sponsor subject tertiarymark tertiarytype url |
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7. Description control | |
e-Mail (login) | simone |
update | |
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