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1. Identity statement
Reference TypeJournal Article
Sitemtc-m16b.sid.inpe.br
Holder Codeisadg {BR SPINPE} ibi 8JMKD3MGPCW/3DT298S
Identifierx6e6X3pFwXQZ3DUS8rS5/BDksu
Repositorycptec.inpe.br/walmeida/2004/04.02.16.24
Last Update2007:11.19.10.03.53 (UTC) administrator
Metadata Repositorycptec.inpe.br/walmeida/2004/04.02.16.24.22
Metadata Last Update2021:02.10.18.35.23 (UTC) administrator
Secondary KeyINPE-10724-PRE/6185
ISSN0894-8755
Citation KeyNobreSellShuk:1991:AmDeRe
TitleAmazonian deforestation and regional climate change
Year1991
MonthOct.
Access Date2024, May 18
Secondary TypePRE PI
Number of Files1
Size2409 KiB
2. Context
Author1 Nobre, Carlos Afonso
2 Sellers, Piers J.
3 Shukla, Jagadish
Resume Identifier1 8JMKD3MGP5W/3C9JGQ7
Group1 CPT-INPE-BR
Affiliation1 Instituto Nacional de Pesquisas Espaciais,(INPE/CPTEC)
2 Center of Ocean-Land-Atmosphere Interactions-COLA, University of Maryland
3 Center of Ocean-Land-Atmosphere Interactions-COLA, University of Maryland
e-Mail Addressdeicy@cptec.inpe.br
JournalJournal of Climate
Volume4
Number10
Pages957-988
History (UTC)2006-03-13 18:35:33 :: Deicy -> administrator ::
2007-03-30 12:03:55 :: administrator -> Deicy ::
2007-11-19 10:03:53 :: Deicy -> administrator ::
2012-11-22 09:56:22 :: administrator -> Deicy :: 1991
2013-02-20 14:52:32 :: Deicy -> administrator :: 1991
2021-02-10 18:35:23 :: administrator -> marciana :: 1991
3. Content and structure
Is the master or a copy?is the master
Content Stagecompleted
Transferable1
Content TypeExternal Contribution
KeywordsAmazonian
deforestation
climate
AbstractLarge-scale conversion of tropical forests into pastures or annual crops could lead to changes in the climate. We have used a coupled numerical model of the global atmosphere and biosphere (Center for Ocean-Land-Atmosphere GCM) to assess the effects of Amazonian deforestation on the regional and global climate. We found that when the Amazonian tropical forests were replaced by degraded grass (pasture) in the model, there was a significant increase in the mean surface temperature (about 2.5-degrees-C) and a decrease in the annual evapotranspiration (30% reduction), precipitation (25% reduction), and runoff (20% reduction) in the region. The differences between the two simulations were greatest during the dry season. The deforested case was associated with larger diurnal fluctuations of surface temperature and vapor pressure deficit; such effects have been observed in existing deforested areas in Amazonia. The calculated reduction in precipitation was larger than the calculated decrease in evapotranspiration, indicating a reduction in the regional moisture convergence. There was also an increase in the length of the dry season in the southern half of the Amazon Basin, which could have serious implications for the reestablishment of the tropical forests following massive deforestation since rainforests only occur where the dry season is very short or nonexistent. An empirical bioclimatic scheme based on an integrated soil moisture stress index was used to derive the movement of the savanna-forest boundary in response to the simulated climate change produced by large-scale deforestation. The implications of possible climate changes in adjacent regions are discussed.
AreaMET
Arrangementurlib.net > BDMCI > Fonds > Produção anterior à 2021 > CGCPT > Amazonian deforestation and...
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4. Conditions of access and use
data URLhttp://mtc-m16b.sid.inpe.br/ibi/x6e6X3pFwXQZ3DUS8rS5/BDksu
zipped data URLhttp://mtc-m16b.sid.inpe.br/zip/x6e6X3pFwXQZ3DUS8rS5/BDksu
Languageen
Target Fileamazonian_deforestation.pdf
User GroupDeicy
administrator
Visibilityshown
Copy HolderSID/SCD
Archiving Policydenypublisher6 allowfinaldraft
Read Permissionallow from all
5. Allied materials
Next Higher Units8JMKD3MGPCW/3EUPEJL
Citing Item Listsid.inpe.br/bibdigital/2013/10.06.18.03 1
DisseminationWEBSCI; PORTALCAPES; AGU; MGA; COMPENDEX.
Host Collectioncptec.inpe.br/walmeida/2003/04.25.17.12
6. Notes
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7. Description control
e-Mail (login)marciana
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