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1. Identificação
Tipo de ReferênciaArtigo em Revista Científica (Journal Article)
Sitemtc-m21d.sid.inpe.br
Código do Detentorisadg {BR SPINPE} ibi 8JMKD3MGPCW/3DT298S
Identificador8JMKD3MGP3W34T/4ATGG5E
Repositóriosid.inpe.br/mtc-m21d/2024/03.14.18.02
Última Atualização2024:03.14.18.02.53 (UTC) simone
Repositório de Metadadossid.inpe.br/mtc-m21d/2024/03.14.18.02.53
Última Atualização dos Metadados2024:03.24.08.21.48 (UTC) administrator
DOI10.3390/atmos15020182
ISSN2073-4433
Chave de CitaçãoRibeiroMRECAGO:2024:RaLiSy
TítuloRadar, Lightning, and Synoptic Observations for a Thunderstorm on 7 January 2012 during the CHUVA-Vale Campaign
Ano2024
MêsFeb.
Data de Acesso17 jun. 2024
Tipo de Trabalhojournal article
Tipo SecundárioPRE PI
Número de Arquivos1
Tamanho11298 KiB
2. Contextualização
Autor1 Ribeiro, João Gabriel Martins
2 Mattos, Enrique Vieira
3 Reboita, Michelle Simões
4 Enore, Diego Pereira
5 Costa, Izabelly Carvalho da
6 Albrecht, Rachel Ifanger
7 Gonçalves, Weber Andrade
8 Oliveira, Romulo Augusto Juca
ORCID1 0000-0002-9854-8693
2 0000-0002-9590-3709
3
4
5
6 0000-0003-0582-6568
7
8 0000-0001-5090-1817
Grupo1
2
3
4 DIPTC-CGCT-INPE-MCTI-GOV-BR
5 DIPTC-CGCT-INPE-MCTI-GOV-BR
Afiliação1 Universidade Federal de Itajubá (UNIFEI)
2 Universidade Federal de Itajubá (UNIFEI)
3 Universidade Federal de Itajubá (UNIFEI)
4 Instituto Nacional de Pesquisas Espaciais (INPE)
5 Instituto Nacional de Pesquisas Espaciais (INPE)
6 Universidade de São Paulo (USP)
7 Universidade Federal do Rio Grande do Norte (UFRN)
8 Géosciences Environnement Toulouse (GET)
Endereço de e-Mail do Autor1 gabrielmr472@unifei.edu.br
2 enrique@unifei.edu.br
3 reboita@unifei.edu.br
4 diegoenore@gmail.com
5 izabelly.costa@inpe.br
6 rachel.albrecht@iag.usp.br
7 goncalves.weber@gmail.com
8 rom.aug9@gmail.com
RevistaAtmosphere
Volume15
Número2
Páginase182
Nota SecundáriaB3_ENGENHARIAS_III B3_ENGENHARIAS_I B3_CIÊNCIAS_AMBIENTAIS B4_ENGENHARIAS_II B5_GEOCIÊNCIAS
Histórico (UTC)2024-03-14 18:02:53 :: simone -> administrator ::
2024-03-14 18:02:55 :: administrator -> simone :: 2024
2024-03-14 18:04:09 :: simone -> administrator :: 2024
2024-03-24 08:21:48 :: administrator -> simone :: 2024
3. Conteúdo e estrutura
É a matriz ou uma cópia?é a matriz
Estágio do Conteúdoconcluido
Transferível1
Tipo do ConteúdoExternal Contribution
Tipo de Versãopublisher
Palavras-Chavehailstorm
synoptic environment
thunderstorm electrical structure
cloud microphysical
southern Brazil
ResumoThunderstorms can generate intense electrical activity, hail, and result in substantial economic and human losses. The development of very short-term forecasting tools (nowcasting) is essential to provide information to alert systems in order to mobilize most efficiently the population. However, the development of nowcasting tools depends on a better understanding of the physics and microphysics of clouds and lightning formation and evolution. In this context, the objectives of this study are: (a) to describe the environmental conditions that led to a genesis of a thunderstorm that produce hail on 7 January 2012, in the Metropolitan Area of Sao Paulo (MASP) during the CHUVA-Vale campaign, and (b) to evaluate the thunderstorm microphysical properties and vertical structure of electrical charge. Data from different sources were used: field campaign data, such as S-band radar, and 2- and 3-dimensional lightning networks, satellite data from the Geostationary Operational Environmental Satellite-13 (GOES-13), the Meteosat Second Generation (MSG), and reanalysis of the European Centre for Medium-Range Weather Forecasts Reanalysis v5 (ERA5). The thunderstorm developed in a region of low-pressure due to the presence of a near-surface inverted trough and moisture convergence, which favored convection. Convective Available Potential Energy (CAPE) of 1053.6 J kg-1 at the start of the thunderstorm indicated that strong convective energy was present. Microphysical variables such as Vertically Integrated Liquid water content (VIL) and Vertically Integrated Ice (VII) showed peaks of 140 and 130 kg m-2, respectively, before the hail reached the surface, followed by a decrease, indicating content removal from within the clouds to the ground surface. The thunderstorm charge structure evolved from a dipolar structure (with a negative center between 4 and 6 km and a positive center between 8 and 10 km) to a tripolar structure (negative center between 6 and 7.5 km) in the most intense phase. The first lightning peak (100 flashes in 5 min-1) before the hail showed that there had been a lightning jump. The maximum lightning occurred around 18:17 UTC, with approximately 350 flashes 5 min-1 with values higher than 4000 sources 500 m-1 in 5 min-1. Likewise, the vertical cross-sections indicated that the lightning occurred ahead of the thunderstorm's displacement (maximum reflectivity), which could be useful in predicting these events.
ÁreaMET
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4. Condições de acesso e uso
URL dos dadoshttp://urlib.net/ibi/8JMKD3MGP3W34T/4ATGG5E
URL dos dados zipadoshttp://urlib.net/zip/8JMKD3MGP3W34T/4ATGG5E
Arquivo Alvoatmosphere-15-00182-v2.pdf
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5. Fontes relacionadas
Repositório Espelhourlib.net/www/2021/06.04.03.40.25
Unidades Imediatamente Superiores8JMKD3MGPCW/46KUATE
Lista de Itens Citandosid.inpe.br/bibdigital/2022/04.03.22.23 3
DivulgaçãoWEBSCI; PORTALCAPES; SCOPUS.
Acervo Hospedeirourlib.net/www/2021/06.04.03.40
6. Notas
Campos Vaziosalternatejournal archivist callnumber copyholder copyright creatorhistory descriptionlevel e-mailaddress format isbn label language lineage mark nextedition notes parameterlist parentrepositories previousedition previouslowerunit progress project readpermission resumeid rightsholder schedulinginformation secondarydate secondarykey session shorttitle sponsor subject tertiarymark tertiarytype url
7. Controle da descrição
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