| 1. Identity statement | ||||
| Reference Type | Journal Article | |||
| Site | mtc-m21c.sid.inpe.br | |||
| Holder Code | isadg {BR SPINPE} ibi 8JMKD3MGPCW/3DT298S | |||
| Identifier | 8JMKD3MGP3W34R/42EDF48 | |||
| Repository | sid.inpe.br/mtc-m21c/2020/05.05.11.52 (restricted access) | |||
| Last Update | 2020:05.05.11.52.54 (UTC) simone | |||
| Metadata Repository | sid.inpe.br/mtc-m21c/2020/05.05.11.52.54 | |||
| Metadata Last Update | 2022:01.04.01.35.07 (UTC) administrator | |||
| DOI | 10.1016/j.asr.2019.11.024 | |||
| ISSN | 0273-1177 1879-1948 | |||
| Citation Key | ConceiçãoSantosMuReFaAnBaCa:2020:RoTiWi | |||
| Title | On the role of tidal winds in the descending of the high type of sporadic layer (Esh)  | |||
| Year | 2020 | |||
| Month | May | |||
| Access Date | 2024, May 18 | |||
| Type of Work | journal article | |||
| Secondary Type | PRE PI | |||
| Number of Files | 1 | |||
| Size | 7314 KiB | |||
| 2. Context | ||||
| Author | 1 Conceição Santos, Fredson 2 Muella, Marcio Tadeu de Assis Honorato 3 Resende, Laysa Cristina Araújo 4 Fagundes, Paulo Roberto 5 Andrioli, Vânia Fátima 6 Batista, Paulo Prado 7 Carrasco, Alexander José | |||
| Resume Identifier | 1 2 3 4 5 6 8JMKD3MGP5W/3C9JJ3H | |||
| Group | 1 2 3 DIDAE-CGCEA-INPE-MCTIC-GOV-BR 4 5 DIDAE-CGCEA-INPE-MCTIC-GOV-BR 6 DIDAE-CGCEA-INPE-MCTIC-GOV-BR | |||
| Affiliation | 1 Universidade do Vale do Paraíba (UNIVAP) 2 Universidade do Vale do Paraíba (UNIVAP) 3 Instituto Nacional de Pesquisas Espaciais (INPE) 4 Universidade do Vale do Paraíba (UNIVAP) 5 Instituto Nacional de Pesquisas Espaciais (INPE) 6 Instituto Nacional de Pesquisas Espaciais (INPE) 7 Universidad de Los Andes | |||
| Author e-Mail Address | 1 fredcon@ifma.edu.br 2 3 laysa.resende@inpe.br 4 5 vania.andrioli@inpe.br 6 paulo.batista@inpe.br | |||
| Journal | Advances in Space Research | |||
| Volume | 65 | |||
| Number | 9 | |||
| Pages | 2131-2147 | |||
| Secondary Mark | B1_INTERDISCIPLINAR B1_GEOCIÊNCIAS B1_ENGENHARIAS_IV B1_ENGENHARIAS_III B1_BIODIVERSIDADE B3_CIÊNCIA_DA_COMPUTAÇÃO B4_ASTRONOMIA_/_FÍSICA C_CIÊNCIAS_BIOLÓGICAS_I | |||
| History (UTC) | 2020-05-05 11:52:54 :: simone -> administrator :: 2020-05-05 11:52:55 :: administrator -> simone :: 2020 2020-05-05 11:53:23 :: simone -> administrator :: 2020 2020-05-11 00:30:29 :: administrator -> simone :: 2020 2020-06-23 22:58:21 :: simone -> administrator :: 2020 2020-07-08 17:10:55 :: administrator -> simone :: 2020 2020-12-14 13:55:38 :: simone -> administrator :: 2020 2022-01-04 01:35:07 :: administrator -> simone :: 2020 | |||
| 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 | Sporadic layers Tidal winds E-region model Low-latitude ionosphere | |||
| Abstract | As the prevailing tidal winds in the E region are generated by heating mechanisms, the dynamics of Es layers impacted by solar tides is a relevant theme in the space weather studies. This paper aims to identify the tidal wind component involved in the mechanism of formation and descending of the high type of sporadic layer (Esh). The Esh layers observed at altitudes between around 120 and 150 km in the Brazilian low latitude stations of Jataí and São José dos Campos during the months of April, June, September and December of 2016 are used in this analysis. The height variability and altitude descent of the Esh layers are analyzed from the h′Es parameter obtained by ionosonde data. In this study, the observational data are compared with the simulations generated by an extended version of the Ionospheric E-Region Model (MIRE). At higher altitudes in the E region, the results show that the prevailing tidal pattern and wind direction controlling the Esh layer formation and descent are different depending on month: (a) in April and June the zonal wind component and the associated semidiurnal tidal oscillations prevail, with some differences in terms of time of occurrence and descending speeds, and (b) in September and December the diurnal tidal periodicities become dominant, and both the meridional and zonal wind components seem to control the descending of the Esh layers. Since the role of the tidal periodicities and wind directions changed depending on the month, the results suggest a possible seasonal tidal wind pattern, which is not well understood from the present study but requires further investigation. Other relevant aspects of the observations and the modeling are highlighted and discussed. | |||
| Area | CEA | |||
| Arrangement | urlib.net > BDMCI > Fonds > Produção anterior à 2021 > DIDAE > On the role... | |||
| 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 | conceicao-role.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 | |||
| Citing Item List | sid.inpe.br/bibdigital/2013/09.29.20.43 5 | |||
| Dissemination | WEBSCI; PORTALCAPES; 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 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 | ||||