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1. Identificação
Tipo de ReferênciaArtigo em Revista Científica (Journal Article)
Sitemtc-m21b.sid.inpe.br
Código do Detentorisadg {BR SPINPE} ibi 8JMKD3MGPCW/3DT298S
Identificador8JMKD3MGP3W34P/3Q8K3S5
Repositóriosid.inpe.br/mtc-m21b/2017/12.21.11.38
Última Atualização2017:12.21.11.38.40 (UTC) administrator
Repositório de Metadadossid.inpe.br/mtc-m21b/2017/12.21.11.38.40
Última Atualização dos Metadados2021:01.03.02.11.55 (UTC) administrator
DOI10.5194/acp-17-14433-2017
ISSN1680-7316
1680-7324
Chave de CitaçãoBragaRWJAWPVMBAMVMG:2017:FuEvCC
TítuloFurther evidence for CCN aerosol concentrations determining the height of warm rain and ice initiation in convective clouds over the Amazon basin
Ano2017
MêsDec.
Data de Acesso07 maio 2024
Tipo de Trabalhojournal article
Tipo SecundárioPRE PI
Número de Arquivos1
Tamanho6729 KiB
2. Contextualização
Autor 1 Braga, Ramon Campos
 2 Rosenfeld, Daniel
 3 Weigel, Ralf
 4 Jurkat, Tina
 5 Andreae, Meinrat O.
 6 Wendisch, Manfred
 7 Pöschl, Ulrich
 8 Voigt, Christiane
 9 Mahnke, Christoph
10 Borrmann, Stephan
11 Albrecht, Rachel I.
12 Molleker, Sergej
13 Vila, Daniel Alejandro
14 Machado, Luiz Augusto Toledo
15 Grulich, Lucas
Identificador de Curriculo 1
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14 8JMKD3MGP5W/3C9JHMS
Grupo 1 MET-MET-SESPG-INPE-MCTIC-GOV-BR
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13 DIDSA-CGCPT-INPE-MCTIC-GOV-BR
14 DIDSA-CGCPT-INPE-MCTIC-GOV-BR
Afiliação 1 Instituto Nacional de Pesquisas Espaciais (INPE)
 2 The Hebrew University of Jerusalem
 3 Johannes Gutenberg-Universität
 4 Deutsches Zentrum für Luft- und Raumfahrt (DLR)
 5 Max Planck Institute for Chemistry
 6 Universität Leipzig
 7 Max Planck Institute for Chemistry
 8 Johannes Gutenberg-Universität
 9 Johannes Gutenberg-Universität
10 Johannes Gutenberg-Universität
11 Universidade de São Paulo (USP)
12 Max Planck Institute for Chemistry
13 Instituto Nacional de Pesquisas Espaciais (INPE)
14 Instituto Nacional de Pesquisas Espaciais (INPE)
15 Johannes Gutenberg-Universität
Endereço de e-Mail do Autor 1 ramonbraga87@gmail.com
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13 daniel.vila@inpe.br
14 luiz.machado@inpe.br
RevistaAtmospheric Chemistry and Physics
Volume17
Páginas14433-14456
Nota SecundáriaA1_MEDICINA_II A1_INTERDISCIPLINAR A1_GEOCIÊNCIAS A1_ENGENHARIAS_III A1_ENGENHARIAS_I A1_CIÊNCIAS_AMBIENTAIS A1_CIÊNCIAS_AGRÁRIAS_I A2_MATEMÁTICA_/_PROBABILIDADE_E_ESTATÍSTICA A2_ENGENHARIAS_II A2_ASTRONOMIA_/_FÍSICA
Histórico (UTC)2017-12-21 11:38:40 :: simone -> administrator ::
2017-12-21 11:38:41 :: administrator -> simone :: 2017
2017-12-21 11:43:02 :: simone -> administrator :: 2017
2021-01-03 02:11:55 :: administrator -> simone :: 2017
3. Conteúdo e estrutura
É a matriz ou uma cópia?é a matriz
Estágio do Conteúdoconcluido
Transferível1
Tipo do ConteúdoExternal Contribution
Tipo de Versãopublisher
ResumoWe have investigated how aerosols affect the height above cloud base of rain and ice hydrometeor initiation and the subsequent vertical evolution of cloud droplet size and number concentrations in growing convective cumulus. For this purpose we used in situ data of hydrometeor size distributions measured with instruments mounted on HALO aircraft during the ACRIDICONCHUVA campaign over the Amazon during September 2014. The results show that the height of rain initiation by collision and coalescence processes (Dr , in units of meters above cloud base) is linearly correlated with the number concentration of droplets (Nd in cm−3 ) nucleated at cloud base (Dr ≈ 5 · Nd). Additional cloud processes associated with Dr , such as GCCN, cloud, and mixing with ambient air and other processes, produce deviations of ∼ 21 % in the linear relationship, but it does not mask the clear relationship between Dr and Nd, which was also found at different regions around the globe (e.g., Israel and India). When Nd exceeded values of about 1000 cm−3 , Dr became greater than 5000 m, and the first observed precipitation particles were ice hydrometeors. Therefore, no liquid water raindrops were observed within growing convective cumulus during polluted conditions. Furthermore, the formation of ice particles also took place at higher altitudes in the clouds in polluted conditions because the resulting smaller cloud droplets froze at colder temperatures compared to the larger drops in the unpolluted cases. The measured vertical profiles of droplet effective radius (re) were close to those estimated by assuming adiabatic conditions (rea), supporting the hypothesis that the entrainment and mixing of air into convective clouds is nearly inhomogeneous. Additional CCN activation on aerosol particles from biomass burning and air pollution reduced re below rea, which further inhibited the formation of raindrops and ice particles and resulted in even higher altitudes for rain and ice initiation.
ÁreaMET
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4. Condições de acesso e uso
URL dos dadoshttp://mtc-m21b.sid.inpe.br/ibi/8JMKD3MGP3W34P/3Q8K3S5
URL dos dados zipadoshttp://mtc-m21b.sid.inpe.br/zip/8JMKD3MGP3W34P/3Q8K3S5
Idiomaen
Arquivo Alvobraga_further.pdf
Grupo de Usuáriossimone
Grupo de Leitoresadministrator
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Permissão de Atualizaçãonão transferida
5. Fontes relacionadas
Repositório Espelhosid.inpe.br/mtc-m21b/2013/09.26.14.25.22
Unidades Imediatamente Superiores8JMKD3MGPCW/3F35TRS
8JMKD3MGPCW/43SRC6S
Lista de Itens Citandosid.inpe.br/bibdigital/2021/01.03.02.10 3
DivulgaçãoWEBSCI; PORTALCAPES; AGU; SCOPUS.
Acervo Hospedeirosid.inpe.br/mtc-m21b/2013/09.26.14.25.20
6. Notas
Campos Vaziosalternatejournal archivist callnumber copyholder copyright creatorhistory descriptionlevel e-mailaddress format isbn keywords label lineage mark nextedition notes number orcid parameterlist parentrepositories previousedition previouslowerunit progress project readpermission rightsholder schedulinginformation secondarydate secondarykey session shorttitle sponsor subject tertiarymark tertiarytype url
7. Controle da descrição
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