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1. Identity statement
Reference TypeJournal Article
Sitemtc-m16b.sid.inpe.br
Holder Codeisadg {BR SPINPE} ibi 8JMKD3MGPCW/3DT298S
Identifierx6e6X3pFwXQZ3DUS8rS5/BCHTJ
Repositorycptec.inpe.br/walmeida/2004/04.01.16.35
Last Update2005:04.04.03.00.00 (UTC) administrator
Metadata Repositorycptec.inpe.br/walmeida/2004/04.01.16.35.55
Metadata Last Update2022:03.21.19.44.36 (UTC) administrator
Secondary KeyINPE-10708-PRE/6169
ISSN0894-8763
Citation KeyMarengoNobrCulf:1997:ClIm''
TitleClimatic impacts of ''friagens'' in forested and deforested areas of the Amazon basin
Year1997
MonthNov.
Access Date2024, May 18
Secondary TypePRE PI
Number of Files1
Size468 KiB
2. Context
Author1 Marengo, Jose Afonso
2 Nobre, Carlos Afonso
3 Culf, A. D.
Resume Identifier1
2 8JMKD3MGP5W/3C9JGQ7
Group1 CG-INPE-MCT-BR
Affiliation1 CPTEC-INPE-Cacahoeira Paulista-12630-000-SP-Brasil
e-Mail Addressdeicy@cptec.inpe.br
JournalJournal of Applied Meteorology
Volume36
Number11
Pages1553-1556
History (UTC)2005-04-04 12:35:52 :: Deicy -> administrator ::
2012-11-20 04:04:27 :: administrator -> Deicy :: 1997
2013-02-20 14:52:31 :: Deicy -> administrator :: 1997
2022-03-21 19:44:36 :: administrator -> marciana :: 1997
3. Content and structure
Is the master or a copy?is the master
Content Stagecompleted
Transferable1
Content TypeExternal Contribution
AbstractMeteorological observations from the Anglo-Brazilian Amazonian Climate Observation Study (ABRACOS), together with the global reanalysis from the National Center for Environmental Prediction (NCEP) and satellite images, have been used to study the spatial extent and intensity of cold surges (known locally as ''friagens'') in the Amazon basin. Case studies are presented of two of the strongest events of the 1994 winter season: 26 June and 10 July 1994. In both events, daily minimum temperatures in southeastern Brazil dropped to near or below 0 degrees C, while at the same time minimum temperatures in southern Amazonia (Ji-Parana site) were almost 8 degrees C below average. Air temperature and humidity also fell in central and western Amazonia (Manaus and Maraba sites, respectively), although the fact that these reductions were less substantial than those farther to the south indicates that the cold air is greatly modified as it moves across Amazonia. In Ji-Parana the largest drops in minimum temperature coincided with strong winds from the south, implying that cold advection was the main mechanism for the falling temperatures. In contrast, there was no increase in wind speed at Manaus and Maraba during the days with reduced temperatures. At these sites, cooling was due to a reduction of the maximum temperature caused, at least partially, by increased cloudiness rather than by a lowering of minimum temperatures as at Ji-Parana. With regard to the depth of the atmospheric boundary layer (ABL), it is observed that during the passage of the cold air in southern Amazonia, the ABL was cooler and shallower than during the pre-and postfriagem days. The friagens presented are of 5- to 6-day duration, including the passage of the cold front, but the period with cold temperatures lasts between 2 and 3 days.
AreaMET
Arrangementurlib.net > BDMCI > Fonds > Produção anterior à 2021 > CGCPT > Climatic impacts of...
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4. Conditions of access and use
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Languageen
Target FileMarengo_Climatic impacts of friagens in forested.pdf
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5. Allied materials
Next Higher Units8JMKD3MGPCW/3EUPEJL
Citing Item Listsid.inpe.br/bibdigital/2013/10.06.18.03 2
DisseminationWEBSCI; PORTALCAPES.
Host Collectioncptec.inpe.br/walmeida/2003/04.25.17.12
6. Notes
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