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1. Identificação
Tipo de ReferênciaArtigo em Revista Científica (Journal Article)
Siteplutao.sid.inpe.br
Código do Detentorisadg {BR SPINPE} ibi 8JMKD3MGPCW/3DT298S
IdentificadorJ8LNKAN8RW/39RQ9NA
Repositóriodpi.inpe.br/plutao/2011/06.11.02.37.38   (acesso restrito)
Última Atualização2011:06.21.16.50.05 (UTC) administrator
Repositório de Metadadosdpi.inpe.br/plutao/2011/06.11.02.37.39
Última Atualização dos Metadados2021:02.10.18.35.08 (UTC) administrator
Chave SecundáriaINPE--PRE/
DOI10.1016/j.atmosres.2010.11.007
ISSN0169-8095
Rótulolattes: 5379515759830546 2 MattosMach:2011:ClLiMe
Chave de CitaçãoMattosMach:2011:ClLiMe
TítuloCloud-to-ground lightning and Mesoscale Convective Systems
Ano2011
MêsMar.
Data de Acesso03 maio 2024
Tipo SecundárioPRE PI
Número de Arquivos1
Tamanho883 KiB
2. Contextualização
Autor1 Mattos, Enrique Vieira
2 Machado, Luiz Augusto Toledo
Identificador de Curriculo1
2 8JMKD3MGP5W/3C9JHMS
Grupo1 CPT-CPT-INPE-MCT-BR
2 CPT-CPT-INPE-MCT-BR
Afiliação1 Instituto Nacional de Pesquisas Espaciais (INPE)
2 Instituto Nacional de Pesquisas Espaciais (INPE)
Endereço de e-Mail do Autor1 enrique.mattos@cptec.inpe.br
2 machado@cptec.inpe.br
Endereço de e-Mailmachado@cptec.inpe.br
RevistaAtmospheric Research
Volume99
Número3-4
Páginas377-390
Nota SecundáriaB1_ECOLOGIA_E_MEIO_AMBIENTE B1_ENGENHARIAS_II B1_ENGENHARIAS_III B1_GEOCIÊNCIAS A1_INTERDISCIPLINAR
Histórico (UTC)2011-06-11 17:43:43 :: lattes -> administrator :: 2011
2011-06-15 03:37:12 :: administrator -> marciana :: 2011
2011-06-20 18:19:39 :: marciana -> valdirene :: 2011
2011-06-21 17:19:08 :: valdirene -> administrator :: 2011
2011-07-04 17:11:19 :: administrator -> valdirene :: 2011
2011-08-04 13:34:51 :: valdirene -> administrator :: 2011
2011-08-22 08:25:22 :: administrator -> valdirene :: 2011
2011-11-04 12:28:19 :: valdirene -> administrator :: 2011
2021-02-10 18:35:08 :: administrator -> valdirene :: 2011
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-Chaveprevisao imediata
sistema convectivo
lightning
mesoscale convective system
cloud microphysics
nowcasting. LOW-LEVEL JET
SATELLITE INFRARED IMAGERY
SOUTHEASTERN SOUTH-AMERICA
UNITED-STATES
ICE-SCATTERING
RADIATIVE-TRANSFER
CHARGE SEPARATION
WEATHER SYSTEMS
STORM STRUCTURE
MONSOON REGION
ResumoThis work analyzes some physical and microphysical properties of Mesoscale Convective Systems (MCSs) and cloud-to-ground lightning. Satellite data from the GOES-10 infrared and NOAA-18 and TRMM microwave channels and lightning information from the Brazilian lightning detection network (BrasilDAT) were utilized for the period from 2007 to 2009. Based on an automatic MCSs detectionmethod, 720MCSs life cycles were identified during the period and in the region of study, with a lightning detection efficiency of over 90%. During the diurnal cycle, maximum electrical activity occurred close to the time ofmaximum convective cloud fraction (18 UTC), and 3 h after the maximum normalized area expansion rate. Diurnal cycles of both properties were modulated by diurnal heating, and thus could be used to monitor diurnal variability of lightning occurrence. The electrical activity was more intense for the widest (Pearsons correlation of 0.96) and deeper (Pearsons correlation of 0.84) clouds, which reached 390 kmsize and 17 kmmaximumcloud top height. Area growth during the initial phase of MCSs exerted a strong influence on their size and duration, and thus also showed a potential for defining the possibility of electrical activity during their life cycle. The average lightning life cycle exhibited a maximumclose toMCSs maturation, while themaximum average lightning density occurred in the MCSs initial life cycle stage. The growth rate of electrical activity during the early stages can indicate the strength of convection and the possible duration of systems with lightning occurrence. Strong condensation processes and mass flux during the growth phase of the systems can provide favorable conditions for cloud electrification and lightning occurrence. A comparison of high microwave frequencies with lightning data showed a strong relationship of vertically integrated ice content and particle size with lightning occurrence, with Pearson's correlation of 0.86 and 0.96, respectively. The polarization difference in the 85 GHz channel showed that electrical activity increases linearlywith polarization reduction, associated with a high value of Pearson's correlation coefficient (above 0.90). This suggests that regions with more intense electrical activity are predominantly located in areas with a high concentration of larger ice particles that are vertically oriented, due to the existence of intense updrafts and the electric field. These results demonstrate the potential use of thermodynamic, dynamic and microphysical characteristics for analyzing thunderstorms severity, and as additional information for nowcasting and monitoring electrical activity over large regions that lack ground-based lightning sensors.
ÁreaMET
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4. Condições de acesso e uso
Idiomaen
Arquivo AlvoMattos_Cloud.pdf
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marciana
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Política de Arquivamentodenypublisher denyfinaldraft24
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5. Fontes relacionadas
Unidades Imediatamente Superiores8JMKD3MGPCW/3EUPEJL
DivulgaçãoWEBSCI; PORTALCAPES; MGA; COMPENDEX.
Acervo Hospedeirodpi.inpe.br/plutao@80/2008/08.19.15.01
6. Notas
Campos Vaziosalternatejournal archivist callnumber copyholder copyright creatorhistory descriptionlevel format isbn lineage mark mirrorrepository nextedition notes orcid parameterlist parentrepositories previousedition previouslowerunit progress project readergroup rightsholder schedulinginformation secondarydate session shorttitle sponsor subject tertiarymark tertiarytype typeofwork url
7. Controle da descrição
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