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1. Identificação
Tipo de ReferênciaArtigo em Revista Científica (Journal Article)
Sitemarte3.sid.inpe.br
Código do Detentorisadg {BR SPINPE} ibi 8JMKD3MGPCW/3DT298S
Repositóriosid.inpe.br/iris@1905/2005/07.30.02.07.36
Repositório de Metadadossid.inpe.br/iris@1905/2005/07.30.02.07.54
Última Atualização dos Metadados2021:02.10.18.35.59 (UTC) administrator
Chave SecundáriaINPE-9286-PRE/4954
ISSN0377-9971
Rótulo10178
Chave de CitaçãoNobre:1990:ClImAm
TítuloClimatic Impacts of Amazonia Deforestation
FormatoStudy week: Man and His Environment Tropical Forests and Conservation of Species
Ano1990
Data Secundária20021023
Mêsmai.
Data de Acesso07 maio 2024
Tipo SecundárioPRE PI
2. Contextualização
AutorNobre, Carlos Afonso
GrupoCPT-INPE-BR
RevistaPontificiae Academiae Scientiarum Scripta Varia
Volume84
Páginas199-218
Histórico (UTC)2021-02-10 18:35:59 :: administrator -> marciana :: 1990
3. Conteúdo e estrutura
É a matriz ou uma cópia?é a matriz
Estágio do Conteúdoconcluido
Transferível1
Tipo do ConteúdoExternal Contribution
Palavras-ChaveMETEOROLOGIA
ResumoLarge-scale conversion of tropical forests into pastures or annual crops will likely lead to changes in the local microclimate of those regions. Larger diurnal fluctuations of surface temperature and humidity deficit, increased surface runoff during the dry season, and decreased soil moisture are to be expected. It is likely that evapotranspiration will be reduced because of less available radiative energy at the canopy levedl since grass presents a higher albedo than forests, and also due to reduces availability of soil moisture at the rooting zone primarily durein the dry season. Coupled numerical models of the global atmosphere and biosphere have used recently to assess the effects of Amazonia deforestation on the regional and global climate. The results of these General Circulation Model (GCM) simulations show that, if the tropical forests were replaced by degraded grass (pasture) in the model, there was a significant increase in surface temperature and a decrease in evapotranspiration, precipitation and runoff. There was also an increase in the lenght of the dry season which can have serious implications for the reestablishment of the tropical forests in the cleared areas. Global climate changes problaby will occur if there is a markeet chenge in rainfall patterns in tropical forest regions as a result of deforestation. It was also seen that tropical deforestation in Southeast Asia is less likely to cause largescale changes in precipitation of that region. On the other hand, removal of Equatorial Africa's tropical forests might result in equatorward expansion of the semi-arid zones too the north and south of the rainforests.
ÁreaMET
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4. Condições de acesso e uso
IdiomaEn
Grupo de Usuáriosadministrator
Visibilidadeshown
Política de Arquivamentodenypublisher denyfinaldraft
5. Fontes relacionadas
Unidades Imediatamente Superiores8JMKD3MGPCW/3EUPEJL
Acervo Hospedeirosid.inpe.br/banon/2001/04.03.15.36
6. Notas
Campos Vaziosaffiliation alternatejournal archivist callnumber copyholder copyright creatorhistory descriptionlevel dissemination documentstage doi e-mailaddress electronicmailaddress identifier isbn lineage mark mirrorrepository nextedition notes number numberoffiles orcid parameterlist parentrepositories previousedition previouslowerunit progress project readergroup readpermission resumeid rightsholder schedulinginformation secondarymark session shorttitle size sponsor subject targetfile tertiarymark tertiarytype typeofwork url versiontype
7. Controle da descrição
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