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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
Identificador8JMKD3MGP5W34M/3FA4624
Repositóriosid.inpe.br/mtc-m21b/2013/11.26.17.01.32
Última Atualização2014:01.20.11.27.29 (UTC) administrator
Repositório de Metadadossid.inpe.br/mtc-m21b/2013/11.26.17.01.33
Última Atualização dos Metadados2018:06.04.03.14.13 (UTC) administrator
DOI10.1175/JAS-D-12-0231.1
ISSN0022-4928
Rótuloscopus 2013-11
Chave de CitaçãoMakarievaGoNeShNoBuLi:2013:KePhPa
TítuloThe key physical parameters governing frictional dissipation in a precipitating atmosphere
Ano2013
Data de Acesso18 maio 2024
Tipo SecundárioPRE PI
Número de Arquivos1
Tamanho681 KiB
2. Contextualização
Autor1 Makarieva, A. M.
2 Gorshkov, V. G.
3 Nefiodov, A. V.
4 Sheil, D.
5 Nobre, Antonio Donato
6 Bunyard, P.
7 Li, B. -L.
Grupo1
2
3
4
5 CST-CST-INPE-MCTI-GOV-BR
Afiliação1 Theoretical Physics Division, Petersburg Nuclear Physics Institute, St. Petersburg, Russian Federation; XIEG-UCR International Center for Arid Land Ecology, University of California, Riverside, Riverside, CA, United States
2 Theoretical Physics Division, Petersburg Nuclear Physics Institute, St. Petersburg, Russian Federation
3 School of Environmental Science and Management, Southern Cross University, Lismore, NSW, Australia; Institute of Tropical Forest Conservation, Mbarara University of Science and Technology, P.O. Box 44, Kabale, Uganda; Center for International Forestry Research, Bogor, Indonesia
4 Centro de Ciência do Sistema Terrestre/INPE, São José dos Campos, São Paulo, Brazil
5 Instituto Nacional de Pesquisas Espaciais (INPE)
6 University Sergio Arboleda, Bogota, Colombia
7 XIEG-UCR International Center for Arid Land Ecology, University of California, Riverside, Riverside, CA, United States
Endereço de e-Mail do Autor1
2
3
4
5 antonio.nobre@inpe.br
Endereço de e-Mailmarcelo.pazos@inpe.br
RevistaJournal of the Atmospheric Sciences
Volume70
Número9
Páginas2916-2929
Nota SecundáriaA1 A2 B1
Histórico (UTC)2018-06-04 03:14:13 :: administrator -> marcelo.pazos@inpe.br :: 2013
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-ChaveAtmosphere-land interactions
Atmosphere-ocean interactions
Atmospheric circulation
Degree of condensation
Frictional dissipation
Hydrometeorology
Physical parameters
Surface temperatures
Atmospheric temperature
Climatology
Condensation
Estimation
Friction
Surface properties
Turbulence
Water vapor
Tropics
adiabatic process
air temperature
atmosphere-biosphere interaction
atmosphere-hydrosphere interaction
atmospheric circulation
condensation
hydrometeorology
mixing ratio
precipitation (climatology)
relative humidity
turbulence
water vapor
ResumoPrecipitation generates small-scale turbulent air flows-the energy of which ultimately dissipates to heat. The power of this process has previously been estimated to be around 2-4Wm-2 in the tropics: a value comparable in magnitude to the dynamic power of global atmospheric circulation. Here it is suggested that the true value is approximately half the value of this previous estimate. The result reflects a revised evaluation of the mean precipitation pathlength HP. The dependence of HP on surface temperature, relative humidity, temperature lapse rate, and degree of condensation in the ascending air were investigated. These analyses indicate that the degree of condensation, defined as the relative change of the saturated water vapor mixing ratio in the region of condensation, is a major factor determining HP. From this theory the authors develop an estimate indicating that the mean large-scale rate of frictional dissipation associated with total precipitation in the tropics lies between 1 and 2Wm-22 and show empirical evidence in support of this estimate. Under terrestrial conditions frictional dissipation is found to constitute a minor fraction of the dynamic power of condensation-induced atmospheric circulation, which is estimated to be at least 2.5 times larger. However, because HP increases with increasing surface temperature Ts, the rate of frictional dissipation would exceed the power of condensation-induced dynamics, and thus block major circulation, at Ts s 320K in a moist adiabatic atmosphere. © 2013 American Meteorological Society.
ÁreaCST
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Conteúdo da Pasta docacessar
Conteúdo da Pasta sourcenão têm arquivos
Conteúdo da Pasta agreementnão têm arquivos
4. Condições de acesso e uso
URL dos dadoshttp://mtc-m21b.sid.inpe.br/ibi/8JMKD3MGP5W34M/3FA4624
URL dos dados zipadoshttp://mtc-m21b.sid.inpe.br/zip/8JMKD3MGP5W34M/3FA4624
Idiomaen
Grupo de Usuáriosadministrator
marcelo.pazos@inpe.br
Grupo de Leitoresadministrator
marcelo.pazos@inpe.br
Visibilidadeshown
Política de Arquivamentodenypublisher6 allowfinaldraft
Permissão de Leituraallow from all
Permissão de Atualizaçãonão transferida
5. Fontes relacionadas
Repositório Espelhoiconet.com.br/banon/2006/11.26.21.31
Unidades Imediatamente Superiores8JMKD3MGPCW/3F3T29H
Lista de Itens Citandosid.inpe.br/bibdigital/2013/10.19.20.40 1
DivulgaçãoWEBSCI; SCOPUS.
Acervo Hospedeirosid.inpe.br/mtc-m21b/2013/09.26.14.25.20
6. Notas
Campos Vaziosalternatejournal archivist callnumber copyholder copyright creatorhistory descriptionlevel format isbn lineage mark month nextedition notes orcid parameterlist parentrepositories previousedition previouslowerunit progress project resumeid rightsholder schedulinginformation secondarydate secondarykey session shorttitle sponsor subject targetfile tertiarymark tertiarytype typeofwork url
7. Controle da descrição
e-Mail (login)marcelo.pazos@inpe.br
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