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8 referências similares encontradas (inclusive a original) buscando em 17 dentre 17 Arquivos.
Data e hora local de busca: 23/04/2024 05:16.
1. Identificação
Tipo de ReferênciaArtigo em Revista Científica (Journal Article)
Sitemtc-m21b.sid.inpe.br
Código do Detentorisadg {BR SPINPE} ibi 8JMKD3MGPCW/3DT298S
Identificador8JMKD3MGP3W34P/3KB6GH2
Repositóriosid.inpe.br/mtc-m21b/2015/09.28.16.57   (acesso restrito)
Última Atualização2015:09.28.16.59.24 (UTC) administrator
Repositório de Metadadossid.inpe.br/mtc-m21b/2015/09.28.16.57.29
Última Atualização dos Metadados2021:02.04.18.38.38 (UTC) administrator
DOI10.1002/joc.4106
ISSN0899-8418
Rótuloself-archiving-INPE-MCTI-GOV-BR
Chave de CitaçãoTedeschiGrimCava:2015:InCeEa
TítuloInfluence of Central and East ENSO on extreme events of precipitation in South America during austral spring and summer
Ano2015
Data de Acesso23 abr. 2024
Tipo de Trabalhojournal article
Tipo SecundárioPRE PI
Número de Arquivos1
Tamanho13215 KiB
2. Contextualização
Autor1 Tedeschi, Renata Gonçalves
2 Grimm, Alice M.
3 Cavalcanti, Iracema Fonseca de Albuquerque
Identificador de Curriculo1
2
3 8JMKD3MGP5W/3C9JHDE
Grupo1
2
3 DMD-CPT-INPE-MCTI-GOV-BR
Afiliação1 Instituto Nacional de Pesquisas Espaciais (INPE)
2 Universidade Federal do Paraná (UFPR)
3 Instituto Nacional de Pesquisas Espaciais (INPE)
Endereço de e-Mail do Autor1 renata.tedeschi@cptec.inpe.br
2
3 iracema.cavalcanti@inpe.br
RevistaInternational Journal of Climatology
Volume35
Páginas2045-2064
Nota SecundáriaA1_GEOCIÊNCIAS A1_ENGENHARIAS_I A1_CIÊNCIAS_AMBIENTAIS A1_CIÊNCIAS_AGRÁRIAS_I A2_INTERDISCIPLINAR A2_BIODIVERSIDADE B1_CIÊNCIAS_BIOLÓGICAS_I
Histórico (UTC)2015-09-28 16:57:29 :: simone -> administrator ::
2021-02-04 18:38:38 :: administrator -> simone :: 2015
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-ChaveCentral and East ENSO
precipitation anomalies
extreme events of precipitation
South America
ResumoRecent studies show that different types of ENSO influence the atmospheric fields differently. In this study, precipitation anomalies and extreme events over South America are analysed with relation to two types of ENSO [East (strong Sea Surface Temperature Anomalies (SSTA) on East Pacific) and Central (strong SSTA on Central Pacific)]. The composites of precipitation anomalies, during these two types of ENSO, show that there are different patterns, e.g. during austral summer of Central El Niño (CEN) there are negative precipitation anomalies in eastern Brazil that do not exist in East El Niño (EEN), whereas in southern Brazil there are positive precipitation anomalies during EEN that do not exist in CEN. Furthermore, the anomalies are mostly stronger and more extensive during EEN (Central La Niña CLN) than in CEN (East La Niña ELN), although there are some exceptions, such as during austral spring in southern Brazil, where anomalies during CEN (ELN) are stronger than during EEN (CLN). The anomalous frequency of extreme precipitation events shows generally patterns consistent with the anomalous precipitation behaviour, though the patterns are not always coincident, because the regions with significant increase of frequency of extreme events tend to be more extensive than those with increased seasonal precipitation. When the monthly or seasonal atmospheric anomalies associated with a type of ENSO episode are very similar (opposite) to the atmospheric anomalies associated with extreme precipitation in a certain region, then a significant enhancement (suppression) of the frequency of extreme events is observed in that region during this type of episode.
ÁreaMET
Arranjourlib.net > BDMCI > Fonds > Produção anterior à 2021 > DIDMD > Influence of Central...
Conteúdo da Pasta docacessar
Conteúdo da Pasta sourcenão têm arquivos
Conteúdo da Pasta agreement
agreement.html 28/09/2015 13:57 1.0 KiB 
4. Condições de acesso e uso
Idiomaen
Arquivo Alvotedeschi_influence.pdf
Grupo de Usuáriossimone
Grupo de Leitoresadministrator
simone
Visibilidadeshown
Política de Arquivamentodenypublisher denyfinaldraft
Permissão de Leituradeny from all and allow from 150.163
Permissão de Atualizaçãonão transferida
5. Fontes relacionadas
Vinculação8JMKD3MGP7W/3DTKRF2
Repositório Espelhosid.inpe.br/mtc-m21b/2013/09.26.14.25.22
Unidades Imediatamente Superiores8JMKD3MGPCW/43SKC35
Lista de Itens Citandosid.inpe.br/bibdigital/2021/01.01.17.20 2
sid.inpe.br/mtc-m21/2012/07.13.14.50.18 1
DivulgaçãoWEBSCI; PORTALCAPES; COMPENDEX; SCOPUS.
Acervo Hospedeirosid.inpe.br/mtc-m21b/2013/09.26.14.25.20
6. Notas
Campos Vaziosalternatejournal archivist callnumber copyholder copyright creatorhistory descriptionlevel e-mailaddress format isbn lineage mark month nextedition notes number orcid parameterlist parentrepositories previousedition previouslowerunit progress project rightsholder schedulinginformation secondarydate secondarykey session shorttitle sponsor subject tertiarytype url
7. Controle da descrição
e-Mail (login)simone
atualizar 

1. Identificação
Tipo de ReferênciaArtigo em Revista Científica (Journal Article)
Siteplutao.sid.inpe.br
Código do Detentorisadg {BR SPINPE} ibi 8JMKD3MGPCW/3DT298S
Identificador8JMKD3MGP3W/3HG7PA9
Repositóriosid.inpe.br/plutao/2014/12.01.14.16.55   (acesso restrito)
Última Atualização2015:01.15.16.01.27 (UTC) administrator
Repositório de Metadadossid.inpe.br/plutao/2014/12.01.14.16.56
Última Atualização dos Metadados2021:01.02.03.53.00 (UTC) administrator
DOI10.1002/joc.4106
ISSN0899-8418
Rótulolattes: 6731029375224939 3 TedeschiGrimCava:2014:InCeEa
Chave de CitaçãoTedeschiGrimCava:2014:InCeEa
TítuloInfluence of Central and East ENSO on extreme events of precipitation in South America during austral spring and summer
Ano2014
Data de Acesso23 abr. 2024
Tipo de Trabalhojournal article
Tipo SecundárioPRE PI
Número de Arquivos1
Tamanho13273 KiB
2. Contextualização
Autor1 Tedeschi, Renata Gonçalves
2 Grimm, Alice M.
3 Cavalcanti, Iracema Fonseca de Albuquerque
Identificador de Curriculo1
2
3 8JMKD3MGP5W/3C9JHDE
Grupo1 MET-MET-SPG-INPE-MCTI-GOV-BR
2
3 DMD-CPT-INPE-MCTI-GOV-BR
Afiliação1 Instituto Nacional de Pesquisas Espaciais (INPE)
2
3 Instituto Nacional de Pesquisas Espaciais (INPE)
Endereço de e-Mailmarcelo.pazos@inpe.br
RevistaInternational Journal of Climatology
Volume1
Páginasn/a-n/a
Nota SecundáriaA1_CIÊNCIAS_AGRÁRIAS_I A1_ENGENHARIAS_I A1_CIÊNCIAS_AMBIENTAIS A1_GEOCIÊNCIAS A2_INTERDISCIPLINAR A2_BIODIVERSIDADE B1_CIÊNCIAS_BIOLÓGICAS_I
Histórico (UTC)2014-12-01 14:16:56 :: lattes -> administrator ::
2014-12-10 11:10:57 :: administrator -> lattes :: 2014
2014-12-10 11:14:20 :: lattes -> administrator :: 2014 -> xxxx
2015-01-15 16:01:28 :: administrator :: xxxx -> 2014
2021-01-02 03:53:00 :: administrator -> marcelo.pazos@inpe.br :: 2014
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-Chaveextreme precipitation
ENSO
ResumoRecent studies show that different types of ENSO influence the atmospheric fields differently. In this study, precipitation anomalies and extreme events over South America are analysed with relation to two types of ENSO [East (strong Sea Surface Temperature Anomalies (SSTA) on East Pacific) and Central (strong SSTA on Central Pacific)]. The composites of precipitation anomalies, during these two types of ENSO, show that there are different patterns, e.g. during austral summer of Central El Niño (CEN) there are negative precipitation anomalies in eastern Brazil that do not exist in East El Niño (EEN), whereas in southern Brazil there are positive precipitation anomalies during EEN that do not exist in CEN. Furthermore, the anomalies are mostly stronger and more extensive during EEN (Central La Niña CLN) than in CEN (East La Niña ELN), although there are some exceptions, such as during austral spring in southern Brazil, where anomalies during CEN (ELN) are stronger than during EEN (CLN). The anomalous frequency of extreme precipitation events shows generally patterns consistent with the anomalous precipitation behaviour, though the patterns are not always coincident, because the regions with significant increase of frequency of extreme events tend to be more extensive than those with increased seasonal precipitation. When themonthly or seasonal atmospheric anomalies associated with a type of ENSO episode are very similar (opposite) to the atmospheric anomalies associated with extreme precipitation in a certain region, then a significant enhancement (suppression) of the frequency of extreme events is observed in that region during this type of episode.
ÁreaMET
Arranjo 1urlib.net > BDMCI > Fonds > Produção pgr ATUAIS > MET > Influence of Central...
Arranjo 2urlib.net > BDMCI > Fonds > Produção anterior à 2021 > DIDMD > Influence of Central...
Conteúdo da Pasta docacessar
Conteúdo da Pasta sourcenão têm arquivos
Conteúdo da Pasta agreementnão têm arquivos
4. Condições de acesso e uso
Idiomaen
Arquivo Alvojoc4106.pdf
Grupo de Usuárioslattes
marcelo.pazos@inpe.br
Grupo de Leitoresadministrator
marcelo.pazos@inpe.br
Visibilidadeshown
Política de Arquivamentodenypublisher denyfinaldraft
Permissão de Leituradeny from all and allow from 150.163
Permissão de Atualizaçãonão transferida
5. Fontes relacionadas
Vinculação8JMKD3MGP7W/3DTKRF2
Unidades Imediatamente Superiores8JMKD3MGPCW/3F35TRS
8JMKD3MGPCW/43SKC35
Lista de Itens Citandosid.inpe.br/bibdigital/2013/10.15.01.34 2
sid.inpe.br/bibdigital/2021/01.01.17.20 1
DivulgaçãoWEBSCI; PORTALCAPES; COMPENDEX; SCOPUS.
Acervo Hospedeirodpi.inpe.br/plutao@80/2008/08.19.15.01
6. Notas
NotasSetores de Atividade: Pesquisa e desenvolvimento científico.
Campos Vaziosalternatejournal archivist callnumber copyholder copyright creatorhistory descriptionlevel electronicmailaddress format isbn lineage mark mirrorrepository month nextedition number orcid parameterlist parentrepositories previousedition previouslowerunit progress project rightsholder schedulinginformation secondarydate secondarykey session shorttitle sponsor subject tertiarytype url
7. Controle da descrição
e-Mail (login)marcelo.pazos@inpe.br
atualizar 

1. Identificação
Tipo de ReferênciaArtigo em Revista Científica (Journal Article)
Siteplutao.sid.inpe.br
Código do Detentorisadg {BR SPINPE} ibi 8JMKD3MGPCW/3DT298S
Identificador8JMKD3MGP3W/3LSCTHG
Repositóriosid.inpe.br/plutao/2016/06.14.12.07.53   (acesso restrito)
Última Atualização2016:12.19.18.47.37 (UTC) lattes
Repositório de Metadadossid.inpe.br/plutao/2016/06.14.12.07.54
Última Atualização dos Metadados2021:01.02.03.53.07 (UTC) administrator
DOI10.1002/joc.4670
ISSN0899-8418
Rótulolattes: 6731029375224939 3 TedeschiGrimCava:2016:InCeEa
Chave de CitaçãoTedeschiGrimCava:2016:InCeEa
TítuloInfluence of Central and East ENSO on precipitation and its extreme events in South America during austral autumn and winter
Ano2016
Data de Acesso23 abr. 2024
Tipo SecundárioPRE PI
Número de Arquivos1
Tamanho11249 KiB
2. Contextualização
Autor1 Tedeschi, Renata G.
2 Grimm, Alice M.
3 Cavalcanti, Iracema Fonseca de Albuquerque
Identificador de Curriculo1
2
3 8JMKD3MGP5W/3C9JHDE
Grupo1
2
3 DMD-CPT-INPE-MCTI-GOV-BR
Afiliação1
2
3 Instituto Nacional de Pesquisas Espaciais (INPE)
RevistaInternational Journal of Climatology
Volume36
Páginasn/a-n/a
Nota SecundáriaA1_GEOCIÊNCIAS A1_ENGENHARIAS_I A1_CIÊNCIAS_AMBIENTAIS A1_CIÊNCIAS_AGRÁRIAS_I A2_INTERDISCIPLINAR A2_BIODIVERSIDADE B1_CIÊNCIAS_BIOLÓGICAS_I
Histórico (UTC)2016-06-14 12:07:54 :: lattes -> administrator ::
2016-06-21 12:56:17 :: administrator -> lattes :: 2016
2016-12-05 21:52:27 :: lattes -> administrator :: 2016
2016-12-15 11:49:44 :: administrator -> lattes :: 2016
2016-12-19 18:47:37 :: lattes -> administrator :: 2016
2021-01-02 03:53:07 :: administrator -> simone :: 2016
3. Conteúdo e estrutura
É a matriz ou uma cópia?é a matriz
Estágio do Conteúdoconcluido
Transferível1
Tipo do ConteúdoExternal Contribution
Tipo de Versãopublisher
ÁreaMET
Arranjourlib.net > Produção anterior à 2021 > DIDMD > Influence of Central...
Conteúdo da Pasta docacessar
Conteúdo da Pasta sourcenão têm arquivos
Conteúdo da Pasta agreementnão têm arquivos
4. Condições de acesso e uso
Idiomaen
Arquivo Alvotedeschi_influence.pdf
Grupo de Leitoresadministrator
lattes
Visibilidadeshown
Política de Arquivamentodenypublisher denyfinaldraft
Permissão de Leituradeny from all and allow from 150.163
Permissão de Atualizaçãonão transferida
5. Fontes relacionadas
Repositório Espelhourlib.net/www/2011/03.29.20.55
Unidades Imediatamente Superiores8JMKD3MGPCW/43SKC35
Lista de Itens Citandosid.inpe.br/mtc-m21/2012/07.13.14.50.18 1
DivulgaçãoWEBSCI; PORTALCAPES; COMPENDEX; SCOPUS.
Acervo Hospedeirodpi.inpe.br/plutao@80/2008/08.19.15.01
6. Notas
Campos Vaziosabstract alternatejournal archivist callnumber copyholder copyright creatorhistory descriptionlevel e-mailaddress electronicmailaddress format isbn keywords lineage mark month nextedition notes number orcid parameterlist parentrepositories previousedition previouslowerunit progress project rightsholder schedulinginformation secondarydate secondarykey session shorttitle sponsor subject tertiarymark tertiarytype typeofwork url usergroup
7. Controle da descrição
e-Mail (login)simone
atualizar 

1. Identificação
Tipo de ReferênciaArtigo em Revista Científica (Journal Article)
Sitemtc-m21d.sid.inpe.br
Código do Detentorisadg {BR SPINPE} ibi 8JMKD3MGPCW/3DT298S
Identificador8JMKD3MGP3W34T/4AGTT95
Repositóriosid.inpe.br/mtc-m21d/2024/01.09.16.35   (acesso restrito)
Última Atualização2024:01.09.16.35.06 (UTC) simone
Repositório de Metadadossid.inpe.br/mtc-m21d/2024/01.09.16.35.06
Última Atualização dos Metadados2024:01.15.20.38.57 (UTC) administrator
DOI10.1016/j.dynatmoce.2023.101422
ISSN0377-0265
Chave de CitaçãoLaureantiChouNobrCurc:2024:ReThSo
TítuloOn the relationship between the South Atlantic Convergence Zone and sea surface temperature during Central-East Brazil extreme precipitation events
Ano2024
MêsMar.
Data de Acesso23 abr. 2024
Tipo de Trabalhojournal article
Tipo SecundárioPRE PI
Número de Arquivos1
Tamanho8282 KiB
2. Contextualização
Autor1 Laureanti, Nicole Crisine
2 Chou, Sin Chan
3 Nobre, Paulo
4 Curchitser, Enrique
Identificador de Curriculo1
2
3 8JMKD3MGP5W/3C9JJ3B
Grupo1 MET-MET-DIPGR-INPE-MCTI-GOV-BR
2 DIMNT-CGCT-INPE-MCTI-GOV-BR
3 DIMNT-CGCT-INPE-MCTI-GOV-BR
Afiliação1 Instituto Nacional de Pesquisas Espaciais (INPE)
2 Instituto Nacional de Pesquisas Espaciais (INPE)
3 Instituto Nacional de Pesquisas Espaciais (INPE)
4 The State University of New Jersey
Endereço de e-Mail do Autor1 nicole.laureanti@inpe.br
2 chou.chan@inpe.br
3 paulo.nobre@inpe.br
RevistaDynamics of Atmospheres and Oceans
Volume105
Páginase101422
Nota SecundáriaA2_GEOCIÊNCIAS
Histórico (UTC)2024-01-09 16:35:06 :: simone -> administrator ::
2024-01-09 16:35:09 :: administrator -> simone :: 2024
2024-01-09 16:35:40 :: simone -> administrator :: 2024
2024-01-15 20:38:57 :: administrator -> simone :: 2024
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-ChaveOcean-atmosphere interactions
Precipitation extremes
South Atlantic Convergence Zone
South Atlantic Ocean
ResumoThe precipitation in Central-East Brazil (CEB) from December to February is heavily influenced by the South Atlantic Convergence Zone (SACZ). The SACZ not only causes considerable rainfall but also has an impact on the underlying ocean. This study examines the extreme precipitation events in CEB and their relationship with the SACZ and sea surface temperature (SST). Empirical Orthogonal Function (EOF) analyses of daily precipitation and vertical velocity at 500 hPa data diagnose the extremes. The grouped events of similar positioning and intensity resulted in 170 extremely wet and 172 dry events. Results indicate that the variability of the SACZ is responsible for extremely wet precipitation events in CEB. Composites of precipitation, SST, and wind anomalies at 850-hPa and 200-hPa characterize their occurrence and resemble SACZ high-intensity variability. Conversely, extremely dry CEB conditions are associated with SACZ southern events (51 events) and SACZ inactivity (121 events). The latter refers to major drought events when upper-level cyclonic circulation favors dry air descending and inhibiting convection over CEB. SACZ southern events have similar atmospheric dynamical patterns as SACZ events but are displaced to the south. The meridional displacement of the South Atlantic Low-Level Jet (SALLJ) and its confluence with the northeasterly flow of the South Atlantic Subtropical High (SASH) are identified as the causes of the cooling or heating of the underlying ocean. The intensity of the extreme event is related to the strength of lower-level wind circulation, while upper-level wind circulation anomalies favor the lower-level effects. The persistence of the systems is related to the development of SST anomalies.
ÁreaMET
ArranjoFonds > Produção a partir de 2021 > CGCT > On the relationship...
Conteúdo da Pasta docacessar
Conteúdo da Pasta sourcenão têm arquivos
Conteúdo da Pasta agreement
agreement.html 09/01/2024 13:35 1.0 KiB 
4. Condições de acesso e uso
Idiomaen
Arquivo Alvo1-s2.0-S0377026523000738-main.pdf
Grupo de Usuáriossimone
Grupo de Leitoresadministrator
simone
Visibilidadeshown
Política de Arquivamentodenypublisher denyfinaldraft24
Permissão de Leituradeny from all and allow from 150.163
Permissão de Atualizaçãonão transferida
5. Fontes relacionadas
Repositório Espelhourlib.net/www/2021/06.04.03.40.25
Unidades Imediatamente Superiores8JMKD3MGPCW/3F35TRS
8JMKD3MGPCW/46KUATE
Lista de Itens Citandosid.inpe.br/bibdigital/2013/10.15.01.34 2
DivulgaçãoWEBSCI
Acervo Hospedeirourlib.net/www/2021/06.04.03.40
6. Notas
Campos Vaziosalternatejournal archivist callnumber copyholder copyright creatorhistory descriptionlevel e-mailaddress format isbn label lineage mark nextedition notes number orcid parameterlist parentrepositories previousedition previouslowerunit progress project rightsholder schedulinginformation secondarydate secondarykey session shorttitle sponsor subject tertiarymark tertiarytype url
7. Controle da descrição
e-Mail (login)simone
atualizar 

1. Identificação
Tipo de ReferênciaArtigo em Evento (Conference Proceedings)
Sitemtc-m16b.sid.inpe.br
Código do Detentorisadg {BR SPINPE} ibi 8JMKD3MGPCW/3DT298S
Repositóriocptec.inpe.br/adm_conf/2005/10.27.22.06
Última Atualização2006:04.16.18.41.54 (UTC) administrator
Repositório de Metadadoscptec.inpe.br/adm_conf/2005/10.27.22.07
Última Atualização dos Metadados2018:06.05.03.42.48 (UTC) administrator
Chave de CitaçãoBerriBert:2006:DiStEn
TítuloDiagnostic study of Enso modulation of low-level southward moisture flux across central South America during summer and its related precipitation
FormatoCD-ROM, On-line.
Ano2006
Data de Acesso23 abr. 2024
Tipo SecundárioPRE CI
Número de Arquivos1
Tamanho3148 KiB
2. Contextualização
Autor1 Berri, Guillermo J.
2 Bertossa, German
Afiliação1 Department of Atmospheric and Oceanic Sciences, University of Buenos Aires, Buenos Aires, Argentina
Endereço de e-Mail do Autor1 berri@at.fcen.uba.ar
EditorVera, Carolina
Nobre, Carlos
Endereço de e-Mailberri@at.fcen.uba.ar
Nome do EventoInternational Conference on Southern Hemisphere Meteorology and Oceanography, 8 (ICSHMO).
Localização do EventoFoz do Iguaçu
Data24-28 Apr. 2006
Editora (Publisher)American Meteorological Society (AMS)
Cidade da Editora45 Beacon Hill Road, Boston, MA, USA
Páginas967-975
Título do LivroProceedings
Tipo TerciárioPoster
OrganizaçãoAmerican Meteorological Society (AMS)
Histórico (UTC)2005-10-27 22:07:00 :: berri@at.fcen.uba.ar -> adm_conf ::
2005-12-16 02:07:46 :: adm_conf -> administrator ::
2005-12-16 02:15:31 :: administrator -> berri@at.fcen.uba.ar ::
2006-03-13 20:50:12 :: berri@at.fcen.uba.ar -> administrator ::
2006-04-18 20:59:16 :: administrator -> lise@dpi.inpe.br ::
2010-12-28 12:36:26 :: lise@dpi.inpe.br -> administrator ::
2010-12-29 15:56:11 :: administrator -> lise@dpi.inpe.br :: 2006
2010-12-29 16:05:47 :: lise@dpi.inpe.br -> administrator :: 2006
2010-12-29 18:52:01 :: administrator -> banon :: 2006
2011-01-02 17:14:47 :: banon -> administrator :: 2006
2018-06-05 03:42:48 :: administrator -> :: 2006
3. Conteúdo e estrutura
É a matriz ou uma cópia?é a matriz
Estágio do Conteúdoconcluido
Transferível1
Palavras-ChaveEnso modulation
low-level moisture
summertime meridional transport
central South America
ResumoThe ENSO modulation during summertime -October through March- of the low-level meridional moisture flux across Central South America -CESA- is studied by means of El Niño -EN- and La Niña -LN- composites of the NCEP/NCAR reanalysis and EUA_CRU precipitation database during recent decades. The period October-March of EN events is characterized by positive precipitation anomalies over northern Argentina, most of Paraguay, Uruguay and the extreme south of Brazil, and a well-defined anomalous moisture influx into northern and central Argentina, more marked during November, December and March. In January there seems to be a bifurcation of the water vapor flux anomalies coming from the NW into northern CESA, which directs moisture towards the east, into central-east Brazil, and to the south into northern Argentina, the two places which show positive precipitation anomalies. In a regional context, the period is characterized by the enhancement of the climatological water vapor flux (except in October), i.e. inflow over the northeastern part of the continent, counterclockwise shift and southeastward extension up to the midlatitudes of South America. The largest anomalies appear over a NW-SE moisture corridor across CESA. Over the eastern side of the continent, at tropical latitudes, the anomalies are very small and only important, in comparison to those at equatorial latitudes, during January (reduced influx) and February and March (enhanced influx). Over the northern part of the continent there is a reduced water valor influx in every month except October. During the same period of LN events, the conditions over the southern half of CESA are opposite to those observed during EN (except for January and February). The situation is now characterized by precipitation deficit and southwesterly water vapor flux anomalies (i.e. reduced northeasterly moisture influx). Instead January, and to a lesser degree February, display positive precipitation anomalies similar to those observed during EN events. In particular, January presents the largest observed water vapor flux anomalies. Over eastern CESA there is enhanced NW-SE moisture influx in coincidence with large positive precipitation anomalies. In a regional context the period is characterized by reduced moisture influx over northeastern South America and to a lesser degree over the north, in particular from December through March. Thus, over northern South America the water vapor flux anomalies during EN and LN behave in an opposite way. Over the eastern side of the continent, at tropical latitudes, there is reduced moisture influx anomalies that combined with the enhancement of the northwesterly moisture corridor that crosses CESA, create a large low-level anticyclonic circulation anomaly.
ÁreaMET
TipoMonsoon systems and continental rainfall
Conteúdo da Pasta docacessar
Conteúdo da Pasta source
PaperFlujosaEnviar.doc 13/03/2006 17:50 2.7 MiB
Conteúdo da Pasta agreementnão têm arquivos
4. Condições de acesso e uso
URL dos dadoshttp://urlib.net/ibi/cptec.inpe.br/adm_conf/2005/10.27.22.06
URL dos dados zipadoshttp://urlib.net/zip/cptec.inpe.br/adm_conf/2005/10.27.22.06
Idiomaen
Arquivo Alvo967-976.pdf
Grupo de Usuáriosberri@at.fcen.uba.ar
administrator
Visibilidadeshown
5. Fontes relacionadas
Acervo Hospedeirocptec.inpe.br/nobre/2005/06.02.21.14
cptec.inpe.br/walmeida/2003/04.25.17.12
6. Notas
Nota1
Campos Vaziosarchivingpolicy archivist callnumber contenttype copyholder copyright creatorhistory descriptionlevel dissemination documentstage doi edition group identifier isbn issn label lineage mirrorrepository nextedition nexthigherunit notes numberofvolumes orcid parameterlist parentrepositories previousedition previouslowerunit progress project readergroup readpermission resumeid rightsholder schedulinginformation secondarydate secondarykey secondarymark serieseditor session shorttitle sponsor subject tertiarymark url versiontype volume

1. Identificação
Tipo de ReferênciaArtigo em Evento (Conference Proceedings)
Sitemtc-m21d.sid.inpe.br
Código do Detentorisadg {BR SPINPE} ibi 8JMKD3MGPCW/3DT298S
Identificador8JMKD3MGP3W34T/4B62U2P
Repositóriosid.inpe.br/mtc-m21d/2024/04.17.13.38
Repositório de Metadadossid.inpe.br/mtc-m21d/2024/04.17.13.38.16
Última Atualização dos Metadados2024:04.22.20.07.32 (UTC) administrator
Chave SecundáriaINPE--PRE/
DOI10.5194/egusphere-egu24-12954
Chave de CitaçãoLyraHGSSGQMCCFPF:2024:ExPrEv
TítuloExtreme Precipitation Events in the Northeast Brazil during the winters of 2022 and 2023
Ano2024
Data de Acesso23 abr. 2024
Tipo SecundárioPRE CI
2. Contextualização
Autor 1 Lyra, Matheus
 2 Herdies, Dirceu Luis
 3 Gomes, Helber
 4 Silva, Maria Cristina
 5 Silva, Fabrício
 6 Gomes, Heliofábio
 7 Quadros, Mário
 8 Mantovani Antonio Júnior, José
 9 Coelho, William Ferreira
10 Calvetti, Leonardo
11 Figueroa, Silvio Nilo
12 Pendharkar, Jayant
13 Fernande Neto, Pedro
Identificador de Curriculo 1
 2 8JMKD3MGP5W/3C9JGTU
ORCID 1 0000-0003-0890-762X
 2
 3 0000-0001-9972-9990
Grupo 1
 2 DIIAV-CGCT-INPE-MCTI-GOV-BR
 3
 4
 5
 6
 7
 8 MET-MET-DIPGR-INPE-MCTI-GOV-BR
 9 MET-MET-DIPGR-INPE-MCTI-GOV-BR
10
11 DIMNT-CGCT-INPE-MCTI-GOV-BR
12 DIMNT-CGCT-INPE-MCTI-GOV-BR
Afiliação 1 Universidade Federal de Alagoas (UFAL)
 2 Instituto Nacional de Pesquisas Espaciais (INPE)
 3 Universidade Federal de Alagoas (UFAL)
 4 Universidade Federal de Alagoas (UFAL)
 5 Universidade Federal de Alagoas (UFAL)
 6 Universidade Federal de Alagoas (UFAL)
 7 Instituto Federal de Santa Catarina (IFSC)
 8 Instituto Nacional de Pesquisas Espaciais (INPE)
 9 Instituto Nacional de Pesquisas Espaciais (INPE)
10 Universidade Federal de Pelotas (UFPel)
11 Instituto Nacional de Pesquisas Espaciais (INPE)
12 Instituto Nacional de Pesquisas Espaciais (INPE)
13 Universidade Federal de Campina Grande (UFCG)
Endereço de e-Mail do Autor 1 matheuslyraa@gmail.com
 2 dherdies@gmail.com
 3 helber.gomes@icat.ufal.br
 4 cristina.lemos@icat.ufal.br
 5 fabricio.santos@icat.ufal.br
 6 heliofabio@icat.ufal.br
 7 mquadro95@gmail.com)
 8 jamantovanijr@gmail.com
 9 williamufpel@gmail.com
10 lcalvetti@ufpel.edu.br
11 snilo.figueroa@gmail.com
12
13 piurosfernandes@hotmail.com
Nome do EventoEGU General Assemblyh
Localização do EventoVienna, Austria
Data14-19 Apr. 2024
Título do LivroProceedings
Histórico (UTC)2024-04-17 13:38:16 :: simone -> administrator ::
2024-04-22 20:07:32 :: administrator -> simone :: 2024
3. Conteúdo e estrutura
É a matriz ou uma cópia?é a matriz
Estágio do Conteúdoconcluido
Transferível1
Tipo do ConteúdoExternal Contribution
Tipo de Versãopublisher
ResumoThis study aims to evaluate the synoptic conditions responsible for two extreme precipitation events development that occurred in the same region on the east coast of Northeast Brazil (NEB) in two different years, on July 1, 2022 (185 mm/24h), and July 7, 2023 (213 mm/24h). These events are becoming increasingly frequent in all regions of Brazil, especially in areas with high population density, associated with significant material and human losses, emphasizing the significance of a deeper comprehension of these events. ERA5 global reanalysis data have been used for synoptic and vertical structure evaluation as a first analysis step. Infrared GOES-16 satellite images have been used to monitor the cloudiness development. Pluviometric stations were used to document accumulated precipitation caused by these events. The following step will consist of conducting very high-resolution simulations using the Model for Prediction Across Scales (MPAS) to assess its ability to represent the circulation patterns associated with the analyzed extreme precipitation events. Both analyzed cases occurred along the eastern coast of the NEB, specifically over the Alagoas state, and were triggered by the same synoptic-scale system, the Easterly Wave Disturbances (EWDs). The trough axis penetrating the study area was observed on both examined dates, with a very characteristic relative vorticity of this tropical disturbance. Despite satellite images in the IR channel indicating lower cloud top temperatures in the first case, thermodynamic diagram data showed a greater vertical development of cloudiness in the second case. Distinct situations were observed when analyzing moisture transport convergence fields. In the first event, moisture convergence intensified over 12 hours, while in the second event, moisture convergence over Alagoas was evident throughout the entire day. This variation can be attributed to the intensification of the subtropical anticyclone during the extreme precipitation event in July 2023, which intensified moisture transport in the region. In general, moisture convergence resulted from the high flow of moisture prevailing over the region combined with upward movements caused by the trough present at low levels, which combined with local factors in the region such as topography, contributed to the increase in rainfall over the study area in both analyzed cases.
ÁreaCST
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4. Condições de acesso e uso
Idiomaen
Grupo de Usuáriossimone
Visibilidadeshown
Permissão de Atualizaçãonão transferida
5. Fontes relacionadas
Repositório Espelhourlib.net/www/2021/06.04.03.40.25
Unidades Imediatamente Superiores8JMKD3MGPCW/3F35TRS
8JMKD3MGPCW/46KUATE
Acervo Hospedeirourlib.net/www/2021/06.04.03.40
6. Notas
Campos Vaziosarchivingpolicy archivist callnumber copyholder copyright creatorhistory descriptionlevel dissemination e-mailaddress edition editor format isbn issn keywords label lineage mark nextedition notes numberoffiles numberofvolumes organization pages parameterlist parentrepositories previousedition previouslowerunit progress project publisher publisheraddress readergroup readpermission rightsholder schedulinginformation secondarydate secondarymark serieseditor session shorttitle size sponsor subject targetfile tertiarymark tertiarytype type url volume
7. Controle da descrição
e-Mail (login)simone
atualizar 

1. Identificação
Tipo de ReferênciaArtigo em Evento (Conference Proceedings)
Sitemtc-m16b.sid.inpe.br
Código do Detentorisadg {BR SPINPE} ibi 8JMKD3MGPCW/3DT298S
Repositóriocptec.inpe.br/adm_conf/2005/10.28.18.42
Última Atualização2006:04.16.17.54.28 (UTC) administrator
Repositório de Metadadoscptec.inpe.br/adm_conf/2005/10.28.18.42.31
Última Atualização dos Metadados2021:02.10.19.01.53 (UTC) administrator
Chave SecundáriaINPE-13824-PRE/9010
Chave de CitaçãoRusticucciMarePenaReno:2006:CoObMo
TítuloComparisons between observed and modeled precipitation and temperature extremes in South America during the XX century (IPCC 20C3M)
FormatoCD-ROM; On-line.
Ano2006
Data de Acesso23 abr. 2024
Tipo SecundárioPRE CI
Número de Arquivos1
Tamanho843 KiB
2. Contextualização
Autor1 Rusticucci, Matilde
2 Marengo, José Antonio
3 Penalba, Olga
4 Renom, Madeleine
Grupo1
2 DMD-INPE-MCT-BR
Afiliação1 Departamento de Ciencias de la Atmósfera y los Océanos-FCEN- Universidad de Buenos Aires-Ciudad Universitaria Pab II (1428) Buenos Aires
2 Instituto Nacional de Pesquisas Espaciais (INPE)
3
4 Facultad de Ciencias, Universidad de la República Uruguay
Endereço de e-Mail do Autor1 mati@at.fcen.uba.ar
2 marengo@cptec.inpe.br
3 penalba@at.fcen.uba.ar
4 renom@fisica.edu.uy
EditorVera, Carolina
Nobre, Carlos
Endereço de e-Mailmati@at.fcen.uba.ar
Nome do EventoInternational Conference on Southern Hemisphere Meteorology and Oceanography, 8 (ICSHMO).
Localização do EventoFoz do Iguaçu
Data24-28 Apr. 2006
Editora (Publisher)American Meteorological Society (AMS)
Cidade da Editora45 Beacon Hill Road, Boston, MA, USA
Páginas379-389
Título do LivroProceedings
Tipo TerciárioPoster
OrganizaçãoAmerican Meteorological Society (AMS)
Histórico (UTC)2005-10-28 18:42:32 :: mati@at.fcen.uba.ar -> adm_conf ::
2005-12-15 16:24:09 :: adm_conf -> mati@at.fcen.uba.ar ::
2006-03-28 15:25:39 :: mati@at.fcen.uba.ar -> administrator ::
2006-04-18 21:02:05 :: administrator -> lise@dpi.inpe.br ::
2010-12-28 12:36:29 :: lise@dpi.inpe.br -> administrator ::
2010-12-29 15:56:34 :: administrator -> lise@dpi.inpe.br :: 2006
2010-12-29 16:05:51 :: lise@dpi.inpe.br -> administrator :: 2006
2010-12-29 18:52:22 :: administrator -> banon :: 2006
2011-01-02 17:14:51 :: banon -> administrator :: 2006
2021-02-10 19:01:53 :: administrator -> :: 2006
3. Conteúdo e estrutura
É a matriz ou uma cópia?é a matriz
Estágio do Conteúdoconcluido
Transferível1
Palavras-Chavetemperature extremes
climate change
South America
modelled vs.observed
ResumoOne of the key aspects of Climate Change is to understand the behavior of extremes. It is recognized that the changes in the frequency and intensity of extreme events are likely to have a larger impact than changes in mean climate. We propose to assess the expected changes in climate extremes over southern South America through the analysis of the indices of the IPCC 4th Assessment Model Output for the present climate (IPCC20C3M). These "extreme indices" are derived data, from simulated daily temperature and precipitation, in the form of annual indicator time series. In this paper, for the common period 1960-2000, the mean, standard deviation and mean square error between the grid point from different models and the nearest station was calculated. The indices that could be comparable are: FD: annual occurrence of frost days (days with MinT <0ºC), Tn90: percentage of days where MinT was above the 90th percentile of the 1961-90 base period. R10: number of heavy precipitation days > 10mm (R10), CDD: consecutive dry days and R5D: maximum 5-day precipitation. The available models are CCSM3 (CCSM),USA CNRM-CM3, (CNRM), France GFDL-CM2 .0 (GFDL0) GFDL-CM2.1 (GFDL), USA, INM-CM3.0-Russia (INM), MIROC high-resolution MIROC), MIROC medre-resolution (MIRMED), Japan, and PCM, USA (PCM) In general, it is necessary to think that the values of the models on the Andes cannot be evaluated by the failing of the models in interpreting the orography. If we center the analysis in the Southeast of South America, a low land region which has more dense information, one sees that the average value is well simulated, the station values has similar values over regions, and are of the same order of magnitude, as in case of the models. In some cases, as the model GFDL, FD's average values are well simulated. The interannual variability from days to weeks in average, also is in good agreement. Another temperature extreme, a warm one, Tn90, (being an index percentile-based, is relative to the local climate), It seems to be better represented that the FD. The consecutive dry days are more difficult to be simulated, since the region has a marked precipitation gradient that is not properly represented. The maximums of dryness over central Argentina Andes could not be represented for any model. On the other hand, the extensive dry season of the Amazon, is displeased and exaggerated in GFDL, whereas it does not exist for CCSM3. An index that measures the quantity of extreme rainfall, (R5d) shows in all the models that the quantity of rainfall is underestimated and there the differences of rate of rainfall are not clear. The one that better approaches the average values is the MIROC3.2. When the number of days is evaluated by extreme rainfall (R10), without considering how much it precipitated, the maps are more similar. The Amazon interannual variability is well simulated.
ÁreaMET
TipoClimate change in the SH
ArranjoComparisons between observed...
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4. Condições de acesso e uso
URL dos dadoshttp://urlib.net/ibi/cptec.inpe.br/adm_conf/2005/10.28.18.42
URL dos dados zipadoshttp://urlib.net/zip/cptec.inpe.br/adm_conf/2005/10.28.18.42
Idiomaen
Arquivo Alvo379-390.pdf
Grupo de Usuáriosadministrator
mati@at.fcen.uba.ar
administrator
banon
Visibilidadeshown
Detentor da CópiaSID/SCD
Permissão de Leituraallow from all
5. Fontes relacionadas
Unidades Imediatamente Superiores8JMKD3MGPCW/43SKC35
Acervo Hospedeirocptec.inpe.br/nobre/2005/06.02.21.14
cptec.inpe.br/walmeida/2003/04.25.17.12
6. Notas
Nota1
Campos Vaziosarchivingpolicy archivist callnumber contenttype copyright creatorhistory descriptionlevel dissemination documentstage doi edition identifier isbn issn label lineage mirrorrepository nextedition notes numberofvolumes orcid parameterlist parentrepositories previousedition previouslowerunit progress project readergroup resumeid rightsholder schedulinginformation secondarydate secondarymark serieseditor session shorttitle sponsor subject tertiarymark url versiontype volume

1. Identificação
Tipo de ReferênciaArtigo em Revista Científica (Journal Article)
Sitemtc-m21c.sid.inpe.br
Código do Detentorisadg {BR SPINPE} ibi 8JMKD3MGPCW/3DT298S
Identificador8JMKD3MGP3W34R/3SEP59E
Repositóriosid.inpe.br/mtc-m21c/2018/12.26.11.08   (acesso restrito)
Última Atualização2018:12.26.11.08.13 (UTC) simone
Repositório de Metadadossid.inpe.br/mtc-m21c/2018/12.26.11.08.13
Última Atualização dos Metadados2019:01.14.17.06.41 (UTC) administrator
DOI10.1002/joc.5744
ISSN0899-8418
Chave de CitaçãoAndradeCava:2018:ObAtMo
TítuloAtmospheric characteristics that induce extreme precipitation in frontal systems over Southeastern Brazil during summer: Observations and atmospheric model simulation
Ano2018
MêsNov.
Data de Acesso23 abr. 2024
Tipo de Trabalhojournal article
Tipo SecundárioPRE PI
Número de Arquivos1
Tamanho44396 KiB
2. Contextualização
Autor1 Andrade, Kelen Martins
2 Cavalcanti, Iracema Fonseca de Albuquerque
Identificador de Curriculo1
2 8JMKD3MGP5W/3C9JHDE
ORCID1 0000-0001-5350-581X
2 0000-0002-3890-5767
Grupo1
2 CGCPT-CGCPT-INPE-MCTIC-GOV-BR
Afiliação1 Centro Nacional de Monitoramento e Alertas de Desastres Naturais (CEMADEN)
2 Instituto Nacional de Pesquisas Espaciais (INPE)
Endereço de e-Mail do Autor1 kelen.martins.andrade@gmail.com
2 iracema.cavalcanti@gmail.com
RevistaInternational Journal of Climatology
Volume38
Número14
Páginas5368-5385
Nota SecundáriaA1_GEOCIÊNCIAS A1_ENGENHARIAS_I A1_CIÊNCIAS_AMBIENTAIS A1_CIÊNCIAS_AGRÁRIAS_I A2_INTERDISCIPLINAR A2_BIODIVERSIDADE B1_CIÊNCIAS_BIOLÓGICAS_I
Histórico (UTC)2018-12-26 11:08:43 :: simone -> administrator :: 2018
2019-01-04 16:57:16 :: administrator -> simone :: 2018
2019-01-07 14:41:46 :: simone -> administrator :: 2018
2019-01-07 14:41:47 :: administrator -> simone :: 2018
2019-01-07 14:41:55 :: simone -> administrator :: 2018
2019-01-14 17:06:41 :: administrator -> simone :: 2018
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-ChaveAGCM
atmospheric anomalies
cold fronts
precipitation extremes
South America
ResumoCold fronts are the most frequent synoptic systems that affect Southeast Brazil during the whole year. The highest frequency of these systems at these latitudes occurs in the months of spring (SON) and winter (JJA), but the highest associated precipitation occurs in the spring (SON) and summer (DJF). Some of these fronts present light rains but others cause heavy precipitation, giving rise to flooding and landslides, mainly in the summer. Composites of the two cases (light and heavy rainfall) are analysed for the summer season. Large-scale and regional features are shown to discuss the differences in precipitation. Regional differences are seen in the position and intensity of low pressure and postfrontal high. The differences are also associated with the humidity flux and convergence over the region. The main difference at high levels is the position of the frontal trough, which is close to the region in the wet cases and displaced to the ocean in the dry cases. Features of the Southern Annular Mode and Madden-Julian Oscillation show opposite patterns in the two cases. These modes of variability can modulate extra-tropical wave trains over the Pacific, which have different behaviour downstream, over South America and South Atlantic Ocean. The eddy kinetic energy is stronger over Southeastern Pacific and Southern South America, and wave activity shows energy propagation towards the continent in the wet cases. Similar analyses with results of a global atmospheric model show that the general atmospheric characteristics of a frontal system are reproduced, as the temperature gradient, the wind confluence and the ridge-trough pair associated with the frontal system. The model represents the differences with respect to moisture flux and the frontal trough position, but underestimates the moisture convergence, eddy kinetic energy and wave activity, in the wet cases.
ÁreaMET
Arranjourlib.net > BDMCI > Fonds > Produção anterior à 2021 > CGCPT > Atmospheric characteristics that...
Conteúdo da Pasta docacessar
Conteúdo da Pasta sourcenão têm arquivos
Conteúdo da Pasta agreement
agreement.html 26/12/2018 09:08 1.0 KiB 
4. Condições de acesso e uso
Idiomaen
Arquivo Alvoandrade_atmospheric.pdf
Grupo de Usuáriossimone
Grupo de Leitoresadministrator
simone
Visibilidadeshown
Política de Arquivamentodenypublisher denyfinaldraft
Permissão de Leituradeny from all and allow from 150.163
Permissão de Atualizaçãonão transferida
5. Fontes relacionadas
Unidades Imediatamente Superiores8JMKD3MGPCW/3EUPEJL
Lista de Itens Citandosid.inpe.br/bibdigital/2013/10.06.18.03 3
sid.inpe.br/mtc-m21/2012/07.13.14.50.18 1
DivulgaçãoWEBSCI; PORTALCAPES; COMPENDEX; SCOPUS.
Acervo Hospedeirourlib.net/www/2017/11.22.19.04
6. Notas
Campos Vaziosalternatejournal archivist callnumber copyholder copyright creatorhistory descriptionlevel e-mailaddress format isbn label lineage mark mirrorrepository nextedition notes parameterlist parentrepositories previousedition previouslowerunit progress project rightsholder schedulinginformation secondarydate secondarykey session shorttitle sponsor subject tertiarymark tertiarytype url
7. Controle da descrição
e-Mail (login)simone
atualizar