| 1. Identity statement | ||||
| Reference Type | Journal Article | |||
| Site | mtc-m21c.sid.inpe.br | |||
| Holder Code | isadg {BR SPINPE} ibi 8JMKD3MGPCW/3DT298S | |||
| Identifier | 8JMKD3MGP3W34R/3R3TNMP | |||
| Repository | sid.inpe.br/mtc-m21c/2018/05.07.18.53 (restricted access) | |||
| Last Update | 2018:05.07.18.53.45 (UTC) simone | |||
| Metadata Repository | sid.inpe.br/mtc-m21c/2018/05.07.18.53.45 | |||
| Metadata Last Update | 2021:07.18.04.03.16 (UTC) administrator | |||
| DOI | 10.1016/j.jastp.2017.06.009 | |||
| ISSN | 1364-6826 | |||
| Citation Key | ResendeBaDeBaCaAnMo:2018:InTiWi | |||
| Title | The influence of tidal winds in the formation of blanketing sporadic e-layer over equatorial Brazilian region  | |||
| Year | 2018 | |||
| Month | June | |||
| Access Date | 2024, May 16 | |||
| Type of Work | journal article | |||
| Secondary Type | PRE PI | |||
| Number of Files | 1 | |||
| Size | 2872 KiB | |||
| 2. Context | ||||
| Author | 1 Resende, Laysa Cristina Araújo 2 Batista, Inez Staciarini 3 Denardin, Clezio Marcos 4 Batista, Paulo Prado 5 Carrsco, Alexander José 6 Andrioli, Vânia Fátima 7 Moro, Juliano | |||
| Resume Identifier | 1 2 8JMKD3MGP5W/3C9JHDA 3 4 8JMKD3MGP5W/3C9JJ3H | |||
| Group | 1 DIDAE-CGCEA-INPE-MCTIC-GOV-BR 2 DIDAE-CGCEA-INPE-MCTIC-GOV-BR 3 DIDAE-CGCEA-INPE-MCTIC-GOV-BR 4 DIDAE-CGCEA-INPE-MCTIC-GOV-BR 5 6 DIDAE-CGCEA-INPE-MCTIC-GOV-BR 7 CRCRS-COCRE-INPE-MCTIC-GOV-BR | |||
| Affiliation | 1 Instituto Nacional de Pesquisas Espaciais (INPE) 2 Instituto Nacional de Pesquisas Espaciais (INPE) 3 Instituto Nacional de Pesquisas Espaciais (INPE) 4 Instituto Nacional de Pesquisas Espaciais (INPE) 5 Los Andes University 6 Instituto Nacional de Pesquisas Espaciais (INPE) 7 Instituto Nacional de Pesquisas Espaciais (INPE) | |||
| Author e-Mail Address | 1 laysa.resende@inpe.br 2 inez.batista@inpe.br 3 clezio.denardin@inpe.br 4 paulo.batista@inpe.br 5 layerf2@yahoo.com 6 vania.andrioli@inpe.br 7 juliano.moro@inpe.br | |||
| Journal | Journal of Atmospheric and Solar-Terrestrial Physics | |||
| Volume | 171 | |||
| Pages | 64-71 | |||
| Secondary Mark | A1_ENGENHARIAS_I A2_GEOCIÊNCIAS A2_ENGENHARIAS_III B1_INTERDISCIPLINAR B1_ENGENHARIAS_IV B1_BIODIVERSIDADE B2_ASTRONOMIA_/_FÍSICA C_CIÊNCIAS_BIOLÓGICAS_I | |||
| History (UTC) | 2018-05-07 18:53:45 :: simone -> administrator :: 2018-05-07 18:53:45 :: administrator -> simone :: 2018 2018-05-07 18:56:40 :: simone -> administrator :: 2018 2019-01-04 16:57:05 :: administrator -> simone :: 2018 2019-01-07 12:52:19 :: simone -> administrator :: 2018 2021-07-18 04:03:16 :: administrator -> simone :: 2018 | |||
| 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 | Equatorial aeronomy Blanketing Es layers Es layers model Tidal winds | |||
| Abstract | This work analysis the blanketing sporadic layers (Esb) behavior over São Luís, Brazil (2° 31′ S, 44° 16′ W, dip: −4.80) which is classified as a transition region between equatorial and low-latitude. Hence, some peculiarities can appear as Esb occurrence instead of the common Esq, which is a non-blanketing irregularity layer. The analysis presented here was obtained using a modified version of a theoretical model for the E region (MIRE), which computes the densities of the metallic ions (Fe+ and Mg+) and the densities of the main molecular ions (NO+, O2+, N2+) by solving the continuity and momentum equations for each one of them. In that model, the Es layer physics driven by both diurnal and semidiurnal tidal winds are taken into account and it was extended in height coverage by adding a novel neutral wind model derived from the all-sky meteor radar measurements. Thus, we provide more trustworthy results related to the Es layer formation in the equatorial region. We verified the contribution of each tidal wind component to the Esb layer formation in this equatorial region. Additionally, we compared the Es layer electron density computed by MIRE with the data obtained by using the blanketing frequency parameter (fbEs) deduced from ionograms. The results show that the diurnal component of the tidal wind is more important in the Esb layer formation whereas the semidiurnal component has a little contribution in our simulations. Finally, it was verified that the modified MIRE presented here can be used to study the Esb layers occurrence over the equatorial region in the Brazilian sector. | |||
| Area | CEA | |||
| Arrangement 1 | urlib.net > BDMCI > Fonds > Produção anterior à 2021 > DIDAE > The influence of... | |||
| Arrangement 2 | urlib.net > BDMCI > Fonds > Produção anterior à 2021 > CRCRS > The influence of... | |||
| doc Directory Content | access | |||
| source Directory Content | there are no files | |||
| agreement Directory Content |
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| 4. Conditions of access and use | ||||
| Language | en | |||
| Target File | resende_influence.pdf | |||
| User Group | simone | |||
| Reader Group | administrator simone | |||
| Visibility | shown | |||
| Archiving Policy | denypublisher denyfinaldraft24 | |||
| Read Permission | deny from all and allow from 150.163 | |||
| Update Permission | not transferred | |||
| 5. Allied materials | ||||
| Next Higher Units | 8JMKD3MGPCW/3ETL868 8JMKD3MGPCW/3EUFCFP | |||
| Citing Item List | sid.inpe.br/bibdigital/2013/09.29.20.43 5 sid.inpe.br/mtc-m21/2012/07.13.14.50.14 1 | |||
| Dissemination | WEBSCI; PORTALCAPES; AGU; COMPENDEX; SCOPUS. | |||
| Host Collection | urlib.net/www/2017/11.22.19.04 | |||
| 6. Notes | ||||
| Empty Fields | alternatejournal archivist callnumber copyholder copyright creatorhistory descriptionlevel e-mailaddress format isbn label lineage mark mirrorrepository nextedition notes number orcid parameterlist parentrepositories previousedition previouslowerunit progress project rightsholder schedulinginformation secondarydate secondarykey session shorttitle sponsor subject tertiarymark tertiarytype url | |||
| 7. Description control | ||||
| e-Mail (login) | simone | |||
| update | ||||