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1. Identity statement
Reference TypeJournal Article
Sitemtc-m16b.sid.inpe.br
Holder Codeisadg {BR SPINPE} ibi 8JMKD3MGPCW/3DT298S
Identifierx6e6X3pFwXQZ3DUS8rS5/DKSR7
Repositorycptec.inpe.br/walmeida/2004/10.13.16.39
Last Update2004:12.22.02.00.00 (UTC) administrator
Metadata Repositorycptec.inpe.br/walmeida/2004/10.13.16.39.03
Metadata Last Update2022:03.26.18.00.22 (UTC) administrator
Secondary KeyINPE-11681-PRE/7040
ISSN0894-8755
Citation KeyOyamaNobr:2004:GCSiSt
TitleClimatic consequences of a large-scale desertification in northeast Brazil: A GCM simulation study
Year2004
Monthaug.
Access Date2024, May 18
Secondary TypePRE PI
Number of Files1
Size857 KiB
2. Context
Author1 Oyama, Marcos Daysuke
2 Nobre, Carlos Afonso
Resume Identifier1
2 8JMKD3MGP5W/3C9JGQ7
Group1 DMA-INPE-MCT-BR
Affiliation1 CPTEC-INPE-Cachoeira Paulista-12630-000-SP-Brasil
e-Mail Addressfabia@cptec.inpe.br
JournalJournal of Climate
Volume17
Number16
Pages3203-3213
History (UTC)2006-03-28 19:16:16 :: Fabia -> administrator ::
2008-06-10 19:51:02 :: administrator -> estagiario ::
2010-05-11 16:55:10 :: estagiario -> administrator ::
2022-03-26 18:00:22 :: administrator -> marciana :: 2004
3. Content and structure
Is the master or a copy?is the master
Content Stagecompleted
Transferable1
Content TypeExternal Contribution
Keywordssemi-arid regions
july circulation
biosphere model
global climate
deforestation
albedo
precipitation
vegetation
roughness
dynamics
AbstractThe climatic impacts of a large-scale desertification in northeast Brazil (NEB) are assessed by using the Center for Weather Forecasting and Climate Studies-Center for Ocean-Land-Atmosphere Studies (CPTEC-COLA) AGCM. Two numerical runs are performed. In the control run, NEB is covered by its natural vegetation (most of NEB is covered by a xeromorphic vegetation known as caatinga); in the desertification run, NEB vegetation is changed to desert (bare soil). Each run consists of five 1-yr numerical integrations. The results for NEB wet season (March-May) are analyzed. Desertification results in hydrological cycle weakening: precipitation, evapotranspiration, moisture convergence, and runoff decrease. Surface net radiation decreases and this reduction is almost evenly divided between sensible and latent heat flux. Atmospheric diabatic heating decreases and subsidence anomalies confined at lower atmospheric levels are found. The climatic impacts result from the cooperative action of feedback processes related to albedo increase, plant transpiration suppression, and roughness length decrease. On a larger scale, desertification leads to precipitation increase in the oceanic belt close to the northernmost part of NEB (NNEB). In the NEB-NNEB dipole, the anomalies of vertical motion and atmospheric circulation are confined to lower atmospheric levels, that is, 850-700 hPa. At these levels, circulation anomalies resemble the linear baroclinic response of a shallow atmospheric layer (850-700 hPa) to a tropical heat sink placed over NEB at the middle-layer level. Therefore, NEB climate does show sensitivity to a vegetation change to desert. The present work shows the possibility of significant and pronounced climate impacts, on both regional and large scales, if the environmental degradation in NEB continues unchecked.
AreaMET
Arrangementurlib.net > BDMCI > Fonds > Produção até 2016 > DMA > Climatic consequences of...
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4. Conditions of access and use
data URLhttp://mtc-m16b.sid.inpe.br/ibi/x6e6X3pFwXQZ3DUS8rS5/DKSR7
zipped data URLhttp://mtc-m16b.sid.inpe.br/zip/x6e6X3pFwXQZ3DUS8rS5/DKSR7
Languageen
Target FileOyama_Climatic consequences.pdf
User GroupFabia
administrator
Visibilityshown
Copy HolderSID/SCD
Archiving Policydenypublisher6 allowfinaldraft
Read Permissionallow from all
5. Allied materials
Next Higher Units8JMKD3MGPCW/46JKC45
Citing Item Listsid.inpe.br/bibdigital/2022/03.26.17.47 2
DisseminationWEBSCI; PORTALCAPES; AGU; MGA; COMPENDEX.
Host Collectioncptec.inpe.br/walmeida/2003/04.25.17.12
6. Notes
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7. Description control
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