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3 referências similares encontradas (inclusive a original) buscando em 22 dentre 22 Arquivos.
Data e hora local de busca: 16/05/2024 18:24.
1. Identificação
Tipo de ReferênciaArtigo em Revista Científica (Journal Article)
Siteplutao.sid.inpe.br
Código do Detentorisadg {BR SPINPE} ibi 8JMKD3MGPCW/3DT298S
Identificador8JMKD3MGP3W/3TEQ6PH
Repositóriosid.inpe.br/plutao/2019/06.10.18.43   (acesso restrito)
Última Atualização2019:06.13.13.59.49 (UTC) lattes
Repositório de Metadadossid.inpe.br/plutao/2019/06.10.18.43.01
Última Atualização dos Metadados2021:01.02.22.17.02 (UTC) administrator
DOI10.1038/s41612-019-0061-0
ISSN2397-3722
Rótulolattes: 3214369697732376 6 RaoMaSrFrDaGa:2019:FuInEx
Chave de CitaçãoRaoMaSrFrDaGa:2019:FuInEx
TítuloFuture increase in extreme El Nino events under greenhouse warming increases Zika virus incidence in South America
Ano2019
Data de Acesso16 maio 2024
Tipo de Trabalhojournal article
Tipo SecundárioPRE PI
Número de Arquivos1
Tamanho2229 KiB
2. Contextualização
Autor1 Rao, Vadlamudi Brahmananda
2 Maneesha, K.
3 Sravya, Panangipalli
4 Franchito, Sergio Henrique
5 Dasari, Hariprasad
6 Gan, Manoel Alonso
Identificador de Curriculo1 8JMKD3MGP5W/3C9JJAJ
2
3
4 8JMKD3MGP5W/3C9JJ82
5
6 8JMKD3MGP5W/3C9JHNM
Grupo1 CGCPT-CGCPT-INPE-MCTIC-GOV-BR
2
3
4 CGCPT-CGCPT-INPE-MCTIC-GOV-BR
5
6 DIDOP-CGCPT-INPE-MCTIC-GOV-BR
Afiliação1 Instituto Nacional de Pesquisas Espaciais (INPE)
2 Regional Centre Visakhapatnam
3 King Abdulla University of Science and Technology
4 Instituto Nacional de Pesquisas Espaciais (INPE)
5 King Abdulla University of Science and Technology
6 Instituto Nacional de Pesquisas Espaciais (INPE)
Endereço de e-Mail do Autor1
2
3
4
5
6 manoel.gan@inpe.br
RevistaNPJ Climate and Atmospheric Science
Volume4
Número1
Páginas1-7
Histórico (UTC)2019-06-13 13:59:51 :: lattes -> administrator :: 2019
2021-01-02 22:17:02 :: administrator -> simone :: 2019
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-Chaveevento extremo
ENSO
ZIKA virus
ResumoThe Zika virus (ZIKV) was first found in Zika forest, Uganda in 1947. The disease appeared in the Americas, Northeast Brazil in May 2015. ZIKV propagated rapidly across the Americas and the World Health Organization (WHO) in February 2016 declared this as a public health emergency of international concern. The temperature conditions related to extreme El Niño of 201516 were exceptionally favorable for ZIKV spreading in South America. For the recent spreading of ZIKV, in Americas, Northeast Brazil was the starting point and it was associated with the extreme El Niño 201516. Paz and Semenza found that there is a striking overlap when the regions with extreme climatic conditions in 1 month are juxtaposed with the geographic distribution of ZIKV in subsequent months. They found that the unique climatic conditions generated by extreme El Niño of 201516 are congenial for the dispersal of ZIKV in the Americas. This is not a just coincidence and many authors noted that ZIKV vector Aedes aegypti is strongly dependent on surface climate conditions that occur during extreme El Niño events. Recently a study found that extreme El Niño events will double in future in response to greenhouse warming. Also it was discovered that the increase of extreme El Niño frequency will continue long after 1.5 °C warming stabilization. We analyze future extreme El Niño events along with associated surface temperatures and calculated the ZIKV quantitatively in future extreme El Niño events and found that large parts of South America are highly favorable for the spread of the disease.
ÁreaMET
Arranjo 1urlib.net > BDMCI > Fonds > Produção anterior à 2021 > CGCPT > Future increase in...
Arranjo 2urlib.net > BDMCI > Fonds > Produção anterior à 2021 > DIDOP > Future increase in...
Conteúdo da Pasta docacessar
Conteúdo da Pasta sourcenão têm arquivos
Conteúdo da Pasta agreementnão têm arquivos
4. Condições de acesso e uso
Idiomaen
Arquivo Alvos41612-019-0061-0.pdf
Grupo de Usuárioslattes
Grupo de Leitoresadministrator
lattes
Visibilidadeshown
Permissão de Leituradeny from all and allow from 150.163
Permissão de Atualizaçãonão transferida
5. Fontes relacionadas
Unidades Imediatamente Superiores8JMKD3MGPCW/3EUPEJL
8JMKD3MGPCW/43SQKNE
Lista de Itens Citandosid.inpe.br/mtc-m21/2012/07.13.15.01.10 1
sid.inpe.br/mtc-m21/2012/07.13.15.00 1
sid.inpe.br/bibdigital/2013/10.06.18.03 1
Acervo Hospedeirodpi.inpe.br/plutao@80/2008/08.19.15.01
6. Notas
NotasSetores de Atividade: Pesquisa e desenvolvimento científico.
Campos Vaziosalternatejournal archivingpolicy archivist callnumber copyholder copyright creatorhistory descriptionlevel dissemination e-mailaddress format isbn lineage mark mirrorrepository month nextedition orcid parameterlist parentrepositories previousedition previouslowerunit progress project rightsholder schedulinginformation secondarydate secondarykey secondarymark 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/2005/10.31.22.33
Última Atualização2006:04.15.18.16.42 (UTC) administrator
Repositório de Metadadoscptec.inpe.br/adm_conf/2005/10.31.22.33.36
Última Atualização dos Metadados2018:06.05.03.43.03 (UTC) administrator
Chave de CitaçãoGrimmTede:2006:MeInEl
TítuloMechanisms of the influence of El Niño and La Niña episodes on the frequency of extreme precipitation events in Brazil
FormatoCD-ROM, On-line.
Ano2006
Data de Acesso16 maio 2024
Tipo SecundárioPRE CI
Número de Arquivos1
Tamanho561 KiB
2. Contextualização
Autor1 Grimm, Alice Marlene
2 Tedeschi, Renata Gonçalves
Afiliação1 Universidade Federal do Paraná, Departamento de Física
2 Caixa Postal 19044. 81531-990 Curitiba, PR, Brazil (Grimm
3 Tedeschi)
Endereço de e-Mail do Autor1 grimm@fisica.ufpr.br
2 rgtedeschi@pop.com.br
EditorVera, Carolina
Nobre, Carlos
Endereço de e-Mailgrimm@fisica.ufpr.br
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
Páginas765-773
Título do LivroProceedings
Tipo TerciárioPoster
OrganizaçãoAmerican Meteorological Society (AMS)
Histórico (UTC)2005-10-31 22:33:36 :: grimm@fisica.ufpr.br -> adm_conf ::
2005-12-15 15:36:43 :: adm_conf -> grimm@fisica.ufpr.br ::
2006-03-30 00:21:24 :: grimm@fisica.ufpr.br -> administrator ::
2006-04-18 21:18:11 :: administrator -> lise@dpi.inpe.br ::
2010-12-28 12:36:48 :: lise@dpi.inpe.br -> administrator ::
2010-12-29 15:58:53 :: administrator -> lise@dpi.inpe.br :: 2006
2010-12-29 16:06:13 :: lise@dpi.inpe.br -> administrator :: 2006
2010-12-29 18:54:37 :: administrator -> banon :: 2006
2011-01-02 17:15:13 :: banon -> administrator :: 2006
2018-06-05 03:43:03 :: administrator -> :: 2006
3. Conteúdo e estrutura
É a matriz ou uma cópia?é a matriz
Estágio do Conteúdoconcluido
Transferível1
Palavras-ChaveExtreme events
precipitation
El Niño
La Niña
Brazil
ResumoThis paper examines how El Niño (EN) e La Niña (LN) episodes modify the frequency of extreme precipitation events in Brazil, and the reason for this modification. Gamma distributions were fit to precipitation in each day of the year, in the period 1956-2002, provided by stations all over Brazil. Daily precipitation data are then replaced by their respective percentiles. Extreme events are those with a three-day average percentile above 85. The number of extreme events was computed for each month of each year. Years were classified as EN, LN and normal years, considering, according to the EN/LN cycle, that the year starts in August (year 0) and ends in July (year +1). The mean frequency of extreme events for each month, within each category of year, and the difference between these mean frequencies for EN and normal years, and for LN and normal years show that EN and LN episodes influence significantly the frequency of extreme events in several regions in Brazil during certain periods. The relationships between large-scale atmospheric perturbations and variations in the frequency of extreme precipitation events are sought through composites of anomalous atmospheric fields during extreme events in EN and LN episodes, in three regions in which there is significant change in the frequency of these events. The general features of those anomalous fields are similar, no matter if the extreme events happen during EN or LN episodes or in normal years. They show the essential ingredients for much precipitation: moisture convergence and mechanisms for lifting the air to the condensation level. To understand why the frequency of extreme events varies significantly between EN and LN episodes, we also formed composites of monthly atmospheric anomalous fields during those episodes. In the regions where the frequency of extreme events increases (decreases) the anomaly composites during extreme events show similarity (difference) with respect to the mean anomalies during EN or LN episodes. This indicates that the frequency of extreme events increases (decreases) when the large-scale perturbations favor (hamper) the circulation anomalies associated with them in those regions. This also means that the behavior of the frequency of extreme events is consistent with that of the monthly or seasonal total precipitation. The same conclusion can be reached through the correlation of sea surface temperature (SST) with the monthly precipitation series or the frequency of extreme events for two regions in which these events had their frequency changed during EN and LN episodes. This correlation analysis was carried out to verify whether there is another mechanism responsible for extreme events that does not work during other rainfall events. In general, the relationship between SST and monthly rainfall is similar to the relationship between SST and the frequency of extreme events. There are, however, some differences. For instance, in southern Brazil the frequency of extreme events is correlated both with SST anomalies in the Pacific Ocean (associated with EN/LN) and in the Atlantic Ocean, while the monthly rainfall is more strongly correlated with SST in the Pacific Ocean..
ÁreaMET
TipoHydrological variability and modeling
Conteúdo da Pasta docacessar
Conteúdo da Pasta source
ICSHMO_2006_final_Evex.doc 29/03/2006 21:21 437.5 KiB 
Conteúdo da Pasta agreementnão têm arquivos
4. Condições de acesso e uso
URL dos dadoshttp://mtc-m16b.sid.inpe.br/ibi/cptec.inpe.br/adm_conf/2005/10.31.22.33
URL dos dados zipadoshttp://mtc-m16b.sid.inpe.br/zip/cptec.inpe.br/adm_conf/2005/10.31.22.33
Idiomaen
Arquivo Alvo765-774.pdf
Grupo de Usuáriosgrimm@fisica.ufpr.br
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-m16b.sid.inpe.br
Código do Detentorisadg {BR SPINPE} ibi 8JMKD3MGPCW/3DT298S
Repositóriocptec.inpe.br/adm_conf/2005/10.24.16.24
Última Atualização2006:04.16.19.20.24 (UTC) administrator
Repositório de Metadadoscptec.inpe.br/adm_conf/2005/10.24.16.24.14
Última Atualização dos Metadados2018:06.05.03.42.43 (UTC) administrator
Chave de CitaçãoPscheidtGrim:2006:InElNi
TítuloThe influence of El Niño and La Niña episodes in the occurrence of extreme precipitation events over Southern Brazil
FormatoCD-ROM, On-line.
Ano2006
Data de Acesso16 maio 2024
Tipo SecundárioPRE CI
Número de Arquivos1
Tamanho582 KiB
2. Contextualização
Autor1 Pscheidt, Ieda
2 Grimm, Alice Marlene
Afiliação1 Universidade de São Paulo, Instituto Astronômico, Geofísico e Ciências Atmosféricas, Departamento de Ciências Atmosféricas
2 Rua do Matão, 1226 - Cidade Universitária -05508-900- São Paulo - SP, Brasil (Pscheidt)
3 Universidade Federal do Paraná, Departamento de Física, Centro Politécnico - Campus III - Jardim das Américas - 81531-990 - Curitiba- PR, Brasil (Grimm)
Endereço de e-Mail do Autor1 pscheidt@model.iag.usp.br
2 grimm@fisica.ufpr.br
EditorVera, Carolina
Nobre, Carlos
Endereço de e-Mailpscheidt@model.iag.usp.br
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
Páginas365-370
Título do LivroProceedings
Tipo TerciárioPoster
OrganizaçãoAmerican Meteorological Society (AMS)
Histórico (UTC)2005-10-24 16:24:14 :: pscheidt@model.iag.usp.br -> adm_conf ::
2005-12-16 02:47:42 :: adm_conf -> pscheidt@model.iag.usp.br ::
2006-03-30 00:29:41 :: pscheidt@model.iag.usp.br -> administrator ::
2006-04-18 20:56:26 :: administrator -> lise@dpi.inpe.br ::
2010-12-28 12:36:22 :: lise@dpi.inpe.br -> administrator ::
2010-12-29 15:55:41 :: administrator -> lise@dpi.inpe.br :: 2006
2010-12-29 16:05:43 :: lise@dpi.inpe.br -> administrator :: 2006
2010-12-29 18:51:32 :: administrator -> banon :: 2006
2011-01-02 17:14:43 :: banon -> administrator :: 2006
2018-06-05 03:42:43 :: administrator -> :: 2006
3. Conteúdo e estrutura
É a matriz ou uma cópia?é a matriz
Estágio do Conteúdoconcluido
Transferível1
Palavras-ChaveEl-Niño
extreme events
precipitation
regional analysis
variability
ResumoEl Niño (EN) and La Niña (LN) episodes cause impacts in the precipitation over Southern Brazil. The impact on the frequency of extreme precipitation events is here regionally analysed. November is a period with increase of severe rain events in EN and reduction in LN. During July of the following year also occurs increase/reduction of extreme events in some areas. The precipitation and the number of extreme events in homogeneous areas with respect to significant increase or reduction of severe rain events show significant correlation with Sea Surface Temperature (SST) in some regions of the globe, mainly those affected by El Niño-Southern Oscilation (ENSO) episodes. Notwithstanding, lower-frequency variability is also associated with the variation of these extremes. The variation of the number of severe rain events between different EN and LN episodes seems to be associated with the variation of SST in certain regions. The most recurrent patterns of atmospheric circulation favoring the occurrence of extreme events are present in extreme events during both El Niño and La Niña episodes, as well as during neutral years. However, composites of monthly anomalies in EN and LN years, show that the large-scale favorable conditions for the occurrence of extreme events appear more during EN than during LN episodes. This explains the large difference between the frequency of those events during EN and LN episodes. Composites of anomalies show differences between EN years with more severe rain events and EN years with less of these events with respect to neutral years, mainly in the fields of global SST, vorticity advection at 500 hPa, geopotencial height at 850 hPa, streamfunction at sigma level 0.21 and divergence of vertically integrated moisture flux. These fields show patterns favorable to precipitation during the years with increase in the number of extreme events and unfavorable in years with reduction of these events. During November of EN years with more severe events than normal there is advection of ciclonic vorticity over Southern Brazil and positive SST anomaly in the equatorial East Pacific much more intense than that observed in years with less extreme events. When there is a reduction of extreme precipitation events in July of the year following the onset of an EN episode there are positive anomalies of geopotencial height at low levels and negative at high levels, indicating anomalous subsidence. Furthermore, there are significant negative SST anomalies in the equatorial East Pacific, while in years with more severe events this does not occurr.
ÁreaMET
TipoClimate change in the SH
Conteúdo da Pasta docacessar
Conteúdo da Pasta source
ICSHMO_2006_final_EvextSul.doc 29/03/2006 21:29 634.0 KiB 
Conteúdo da Pasta agreementnão têm arquivos
4. Condições de acesso e uso
URL dos dadoshttp://mtc-m16b.sid.inpe.br/ibi/cptec.inpe.br/adm_conf/2005/10.24.16.24
URL dos dados zipadoshttp://mtc-m16b.sid.inpe.br/zip/cptec.inpe.br/adm_conf/2005/10.24.16.24
Idiomaen
Arquivo Alvo365-370.pdf
Grupo de Usuáriospscheidt@model.iag.usp.br
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