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9 referências similares encontradas (inclusive a original) buscando em 22 dentre 22 Arquivos.
Data e hora local de busca: 16/05/2024 18:05.
1. Identificação
Tipo de ReferênciaArtigo em Revista Científica (Journal Article)
Sitemtc-m21c.sid.inpe.br
Código do Detentorisadg {BR SPINPE} ibi 8JMKD3MGPCW/3DT298S
Identificador8JMKD3MGP3W34R/3SH4R72
Repositóriosid.inpe.br/mtc-m21c/2019/01.09.18.09   (acesso restrito)
Última Atualização2019:01.09.18.09.15 (UTC) simone
Repositório de Metadadossid.inpe.br/mtc-m21c/2019/01.09.18.09.15
Última Atualização dos Metadados2020:01.06.16.45.50 (UTC) simone
DOI10.1002/joc.5812
ISSN0899-8418
Chave de CitaçãoZeriCunGoiLyrOli:2019:ExAsRa
TítuloExposure assessment of rainfall to interannual variability usingthe wavelet transform
Ano2019
Data de Acesso16 maio 2024
Tipo de Trabalhojournal article
Tipo SecundárioPRE PI
Número de Arquivos1
Tamanho4557 KiB
2. Contextualização
Autor1 Zeri, Marcelo
2 Cunha-Zeri, Gisleine da Silva
3 Gois, Givanildo
4 Lyra, Gustavo B.
5 Oliveira Júnior, José Francisco
Grupo1
2 COCST-COCST-INPE-MCTIC-GOV-BR
Afiliação1 Centro Nacional de Monitoramento e Alertas de Desastres Naturais (CEMADEN)
2 Instituto Nacional de Pesquisas Espaciais (INPE)
3 Universidade Federal Fluminense (UFF)
4 Universidade Federal Rural do Rio de Janeiro (UFRRJ)
5 Universidade Federal do Alagoas (UFAL)
Endereço de e-Mail do Autor1
2 gisleine.zeri@inpe.br
RevistaInternational Journal of Climatology
Volume39
Número1
Páginasjan.
Nota SecundáriaA1_GEOCIÊNCIAS A1_ENGENHARIAS_I A1_CIÊNCIAS_AMBIENTAIS A1_CIÊNCIAS_AGRÁRIAS_I A2_INTERDISCIPLINAR A2_BIODIVERSIDADE B1_CIÊNCIAS_BIOLÓGICAS_I
Histórico (UTC)2019-01-09 18:09:15 :: simone -> administrator ::
2019-01-09 18:09:16 :: administrator -> simone :: 2019
2019-01-09 18:10:32 :: simone -> administrator :: 2019
2020-01-06 11:42:08 :: 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
ResumoIt is generally accepted that El NiñoSouthern Oscillation (ENSO) is the main modulator of rainfall variability over Northern South America in the interannual scale. Assuming that, an index is proposed to quantify this expected interannual variability in time series of rainfall. The result is the exposure assessment to the effects of droughts, measured with the Standardized Precipitation Index (SPI) for the monthly scale. The SPI is calculated from rainfall series, and wavelet analysis is used to estimate the variance for different frequencies present in the signal. The Wavelet Interannual Variability Index (WIVI) is calculated as the sum of the wavelet coefficients over a predetermined range of modes of variability (with periods longer than 2 year and shorter than 8 years). The index was tested using a dataset of rainfall records from Tocantins state, Central Brazil. Most of the series ranged from 1974 to 2012. On average, the series had 3.2% of gaps which were not filled to avoid the effect of artificial trends on the data. The state lies mostly over the Cerrado biome and is a new frontier of agricultural development in Brazil. According to the results, the Northern region is under higher exposure of interannual variability, with higher values of WIVI. The assessment is in agreement with large‐scale features of South American climate, specifically considering the influences of the Pacific and Atlantic Oceans and their patterns of sea surface temperature (SST).
ÁreaCST
Arranjourlib.net > BDMCI > Fonds > Produção anterior à 2021 > COCST > Exposure assessment of...
Conteúdo da Pasta docacessar
Conteúdo da Pasta sourcenão têm arquivos
Conteúdo da Pasta agreement
agreement.html 09/01/2019 16:09 1.0 KiB 
4. Condições de acesso e uso
Idiomaen
Arquivo Alvozeri_exposure.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/3F3T29H
Lista de Itens Citandosid.inpe.br/bibdigital/2013/10.19.20.40 4
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 keywords label lineage mark mirrorrepository month nextedition notes orcid parameterlist parentrepositories previousedition previouslowerunit progress project resumeid 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 Revista Científica (Journal Article)
Sitemarte3.sid.inpe.br
Código do Detentorisadg {BR SPINPE} ibi 8JMKD3MGPCW/3DT298S
Identificador6qtX3pFwXQZ3r59YCT/H38uk
Repositóriosid.inpe.br/iris@1905/2005/08.02.22.27
Última Atualização2015:11.18.15.50.25 (UTC) marciana
Repositório de Metadadossid.inpe.br/iris@1905/2005/08.02.22.27.24
Última Atualização dos Metadados2018:06.06.03.54.25 (UTC) administrator
Chave SecundáriaINPE-9099-PRE/4774
ISSN0894-8755
Rótulo6253
Chave de CitaçãoLiebmannMare:2001:InVaRa
TítuloInterannual variability of the rainy season and rainfall in the Brazilian Amazon basin
Ano2001
Data de Acesso16 maio 2024
Tipo SecundárioPRE PI
Número de Arquivos1
Tamanho1624 KiB
2. Contextualização
Autor1 Liebmann, B.
2 Marengo, José Antonio
Grupo1 CPT-INPE-MCT-BR
RevistaJournal of Climate
Volume14
Número22
Páginas4308-4318
Histórico (UTC)2014-09-29 15:09:00 :: administrator -> marciana :: 2001
2015-11-18 15:50:25 :: marciana -> administrator :: 2001
2018-06-06 03:54:25 :: administrator -> marciana :: 2001
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-ChaveESTUDO DO TEMPO E DO CLIMA
South American
Brazilian Amazon basin
sector
surface climate
oscillation
precipitation
convection
ResumoThe interannual variability of deep convection over the South American sector and regional hydrometeorological anomalies are studied using International Satellite Cloud Climatology Project (ISCCP)data for 1984-1988. Satellite-derived convection anomalies are compared with regional rainfall and river runoff anomalies. At the height of the austral summer, the deep convective clouds (DCC)and ISCCP depict the centres of intense convection over central Amazonia and the mouth of the River Amazon, as well as the enhanced convection over north-east Brazil, which is related to the Atlantic Intertropical Convergence Zone (ITCZ). Positive/negative regional hydrometeorological anomalies are consistent with positive/negative anomalies in the deep convection over northern Amazonia, the mouth of the River Amazon and north north-east Brazil, whereas this is not always true over southern Amazonia and southern Brazil. Over north-east Brazil and the mouth of the River Amazon, abundant rainfall and large DCC are both in agreement with variations in the latitudinal position and intensity of the Atlantic ITCZ, which extends between 4 degrees N and 5 degrees S along the Atlantic coast, where the precipitation maximum is found. The related rainfall anomalies over Amazonia and north-east Brazil during years with anomalously warm or cool surface waters in the central equatorial Pacific (e.g. the El Nino event in 1987), are consistent with the convection anomalies as depicted by the ISCCP deep convective clouds. For the Amazon Basin and north-east Brazil, DCC based on 2.5 degrees x 2.5 degrees horizontal resolution explained about 50 per cent of the variance of rainfall at individual surface stations. A new finding is the enhanced convective activity located at the east side of the central Andes and over central Amazonia around 5 degrees S, with a region of reduced convection in between. These two subcentres are oriented west-east and are part of the summertime semi-permanent centre of convection over the Amazon Basin, and have not been identified previously from the analysis of outgoing longwave radiation (OLR)or highly reflective clouds. These subcentres of large DCC exhibit interannual variations in intensity and location, where the centre located near the east flank of the Andes shows a wider range of latitudinal variations than that located over central Amazonia. South of this area convection and rainfall decreases rapidly.
ÁreaMET
Arranjourlib.net > BDMCI > Fonds > Produção anterior à 2021 > CGCPT > Interannual variability of...
Conteúdo da Pasta docacessar
Conteúdo da Pasta sourcenão têm arquivos
Conteúdo da Pasta agreementnão têm arquivos
4. Condições de acesso e uso
URL dos dadoshttp://urlib.net/ibi/6qtX3pFwXQZ3r59YCT/H38uk
URL dos dados zipadoshttp://urlib.net/zip/6qtX3pFwXQZ3r59YCT/H38uk
Arquivo Alvoliebmann.pdf
Grupo de Usuáriosadministrator
marciana
Grupo de Leitoresadministrator
marciana
Visibilidadeshown
Política de Arquivamentodenypublisher6 allowfinaldraft
Permissão de Atualizaçãonão transferida
5. Fontes relacionadas
Unidades Imediatamente Superiores8JMKD3MGPCW/3EUPEJL
Lista de Itens Citandosid.inpe.br/bibdigital/2013/10.06.18.03 2
DivulgaçãoWEBSCI; PORTALCAPES; AGU; MGA; COMPENDEX.
Acervo Hospedeirosid.inpe.br/banon/2001/04.03.15.36
6. Notas
Campos Vaziosaffiliation alternatejournal archivist callnumber copyholder copyright creatorhistory descriptionlevel doi e-mailaddress electronicmailaddress format isbn language lineage mark mirrorrepository month nextedition notes orcid parameterlist parentrepositories previousedition previouslowerunit progress project readpermission resumeid rightsholder schedulinginformation secondarydate secondarymark session shorttitle sponsor subject tertiarymark tertiarytype typeofwork url
7. Controle da descrição
e-Mail (login)marciana
atualizar 

1. Identificação
Tipo de ReferênciaArtigo em Revista Científica (Journal Article)
Sitemtc-m16b.sid.inpe.br
Código do Detentorisadg {BR SPINPE} ibi 8JMKD3MGPCW/3DT298S
Identificador6qtX3pFwXQZ3r59YD9/G3Dzr
Repositóriosid.inpe.br/iris@1915/2005/05.04.14.08
Última Atualização2005:05.04.03.00.00 (UTC) administrator
Repositório de Metadadossid.inpe.br/iris@1915/2005/05.04.14.08.44
Última Atualização dos Metadados2018:06.05.03.52.07 (UTC) administrator
Chave SecundáriaINPE-9099-PRE/4774
ISSN0894-8755
Chave de CitaçãoLiebmannMare:2001:InVaRa
TítuloInterannual variability of the rainy season and rainfall in the Brazilian Amazon basin
Ano2001
Mêsnov.
Data de Acesso16 maio 2024
Tipo SecundárioPRE PI
Número de Arquivos1
Tamanho774 KiB
2. Contextualização
Autor1 Liebmann, B.
2 Marengo, Jose Antonio
Grupo1 CPT-INPE-MCT-BR
Afiliação1 CPTEC-INPE-Cachoeira Paulista-12630-000-SP-Brasil
Endereço de e-Mailatus@cptec.inpe.br
RevistaJournal of Climate
Volume14
Número22
Páginas4308-4318
Histórico (UTC)2005-05-04 14:08:44 :: fabia -> administrator ::
2008-06-10 19:51:45 :: administrator -> estagiario ::
2010-05-11 16:55:56 :: estagiario -> administrator ::
2018-06-05 03:52:07 :: administrator -> marciana :: 2001
3. Conteúdo e estrutura
É a matriz ou uma cópia?é a matriz
Estágio do Conteúdoconcluido
Transferível1
Tipo do ConteúdoExternal Contribution
Palavras-Chaveestudo do tempo e do clima
South American
Brazilian Amazon basin
sector
surface climate
oscillation
precipitation
convection
ResumoThe interannual variability of deep convection over the South American sector and regional hydrometeorological anomalies are studied using International Satellite Cloud Climatology Project (ISCCP)data for 1984-1988. Satellite-derived convection anomalies are compared with regional rainfall and river runoff anomalies. At the height of the austral summer, the deep convective clouds (DCC)and ISCCP depict the centres of intense convection over central Amazonia and the mouth of the River Amazon, as well as the enhanced convection over north-east Brazil, which is related to the Atlantic Intertropical Convergence Zone (ITCZ). Positive/negative regional hydrometeorological anomalies are consistent with positive/negative anomalies in the deep convection over northern Amazonia, the mouth of the River Amazon and north north-east Brazil, whereas this is not always true over southern Amazonia and southern Brazil. Over north-east Brazil and the mouth of the River Amazon, abundant rainfall and large DCC are both in agreement with variations in the latitudinal position and intensity of the Atlantic ITCZ, which extends between 4 degrees N and 5 degrees S along the Atlantic coast, where the precipitation maximum is found. The related rainfall anomalies over Amazonia and north-east Brazil during years with anomalously warm or cool surface waters in the central equatorial Pacific (e.g. the El Nino event in 1987), are consistent with the convection anomalies as depicted by the ISCCP deep convective clouds. For the Amazon Basin and north-east Brazil, DCC based on 2.5 degrees x 2.5 degrees horizontal resolution explained about 50 per cent of the variance of rainfall at individual surface stations. A new finding is the enhanced convective activity located at the east side of the central Andes and over central Amazonia around 5 degrees S, with a region of reduced convection in between. These two subcentres are oriented west-east and are part of the summertime semi-permanent centre of convection over the Amazon Basin, and have not been identified previously from the analysis of outgoing longwave radiation (OLR)or highly reflective clouds. These subcentres of large DCC exhibit interannual variations in intensity and location, where the centre located near the east flank of the Andes shows a wider range of latitudinal variations than that located over central Amazonia. South of this area convection and rainfall decreases rapidly.
ÁreaMET
Arranjourlib.net > BDMCI > Fonds > Produção anterior à 2021 > CGCPT > Interannual variability of...
Conteúdo da Pasta docacessar
Conteúdo da Pasta sourcenão têm arquivos
Conteúdo da Pasta agreementnão têm arquivos
4. Condições de acesso e uso
URL dos dadoshttp://mtc-m16b.sid.inpe.br/ibi/6qtX3pFwXQZ3r59YD9/G3Dzr
URL dos dados zipadoshttp://mtc-m16b.sid.inpe.br/zip/6qtX3pFwXQZ3r59YD9/G3Dzr
Idiomaen
Arquivo AlvoLiebmann_Interannual variability.pdf
Grupo de Usuáriosadministrator
fabia
Visibilidadeshown
Detentor da CópiaSID/SCD
Política de Arquivamentodenypublisher6 allowfinaldraft
Permissão de Leituraallow from all
5. Fontes relacionadas
Unidades Imediatamente Superiores8JMKD3MGPCW/3EUPEJL
Lista de Itens Citandosid.inpe.br/bibdigital/2013/10.06.18.03 1
DivulgaçãoWEBSCI; PORTALCAPES; AGU; MGA; COMPENDEX.
Acervo Hospedeirocptec.inpe.br/walmeida/2003/04.25.17.12
6. Notas
Campos Vaziosalternatejournal archivist callnumber copyright creatorhistory descriptionlevel documentstage doi electronicmailaddress format isbn label lineage mark mirrorrepository nextedition notes orcid parameterlist parentrepositories previousedition previouslowerunit progress project readergroup resumeid rightsholder schedulinginformation secondarydate secondarymark session shorttitle sponsor subject tertiarymark tertiarytype typeofwork url versiontype
7. Controle da descrição
e-Mail (login)marciana
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/2005/10.24.16.12
Última Atualização2006:04.16.19.19.26 (UTC) administrator
Repositório de Metadadoscptec.inpe.br/adm_conf/2005/10.24.16.12.01
Última Atualização dos Metadados2018:06.05.03.42.43 (UTC) administrator
Chave de CitaçãoHirataMöll:2006:PrRe
TítuloInterannual variability of rainfall and streamflow in the Patos Lagoon basin: preliminary results
FormatoCD-ROM, On-line.
Ano2006
Data de Acesso16 maio 2024
Tipo SecundárioPRE CI
Número de Arquivos1
Tamanho392 KiB
2. Contextualização
Autor1 Hirata, Fernando Endo
2 Möller Júnior, Osmar Olinto
Afiliação1 Fundação Universidade Federal do Rio Grande, Laboratório de Oceanografia Física
2 Av. Itália, km 8, s/n, 96201-900, Rio Grande, RS, Brazil (Hirata
3 Möller)
Endereço de e-Mail do Autor1 endohirata@yahoo.com.br
2 dfsomj@furg.br
EditorVera, Carolina
Nobre, Carlos
Endereço de e-Mailendohirata@yahoo.com.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
Páginas775-780
Título do LivroProceedings
Tipo TerciárioPoster
OrganizaçãoAmerican Meteorological Society (AMS)
Histórico (UTC)2005-10-24 16:12:01 :: endohirata@yahoo.com.br -> adm_conf ::
2005-12-16 01:54:49 :: adm_conf -> endohirata@yahoo.com.br ::
2006-03-28 16:27:30 :: endohirata@yahoo.com.br -> administrator ::
2006-04-18 20:56:18 :: administrator -> lise@dpi.inpe.br ::
2010-12-28 12:36:22 :: lise@dpi.inpe.br -> administrator ::
2010-12-29 15:55:40 :: administrator -> lise@dpi.inpe.br :: 2006
2010-12-29 16:05:43 :: lise@dpi.inpe.br -> administrator :: 2006
2010-12-29 18:51:31 :: 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-Chaverainfall and streamflow variability
El-Niño Southern Oscillation
Patos Lagoon
ResumoPatos Lagoon basin (in southern Brazil) has a drainage area of approximately 200,000 km2 and cover almost half of Rio Grande do Sul state. The discharge of the Lagoon is a very important environmental factor for local tourism, fisheries and navigation. To identify variability patterns of rainfall and streamflow in the Patos Lagoon basin and compare them to those found previously for Southeastern South America (SSA), data from 17 rainfall and 3 streamflow stations covering the 1978-2002 period (25 years) were analyzed. Scientific literature describes relations between interannual variability of rainfall in SSA and El-Niño/Southern Oscillation (ENSO) as well as a relationship between the Southern Oscillation (SO) and the streamflow of Negro and Uruguay rivers: lower than average in La Niña (LN) years and higher than average in El Niño (EN) years. Aproximate 3 and 6 years signals, both in the range of variability of the ENSO cycles, were identified as dominant oscillation modes for streamflow in the Uruguay river basin on interanual timescale. For PAtos Lagoon basin, the power spectral density of all series showed peaks that corresponds to periods of 3 and 4 years, in agreement with the relationships between rainfall, streamflow and the SO cited above. Spacial variability were also investigated using other stations located at Rio Grande do Sul state and Empirical Orthogonal Functions (EOF). The first and the second modes of variability are responsible for approximately 65% of the total variance. The first mode (52%) is positive for al the stations and seems to be related to the warm phase of SO (EN), which is associated to positive rainfall anomalies in southern Brazil. The second mode (13%), negative for southern stations, seems to be related to the cold phase of SO (LA - negative anomalies for the region). Applied to the streamflow stations, the EOF showed a first mode that corresponds to 88% of the total variance and is positive for the three major rivers of Patos Lagoon basin (Jacuí, Taquari and Camaquã). The power spectral density of this principal component indicated a dominant peak for approximately 4 year period, probably related to ENSO.
ÁreaMET
TipoHydrological variability and modeling
Conteúdo da Pasta docacessar
Conteúdo da Pasta source
Patos_Lagoon.doc 28/03/2006 13:27 253.5 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/2005/10.24.16.12
URL dos dados zipadoshttp://mtc-m16b.sid.inpe.br/zip/cptec.inpe.br/adm_conf/2005/10.24.16.12
Idiomaen
Arquivo Alvo775-780.pdf
Grupo de Usuáriosendohirata@yahoo.com.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 Revista Científica (Journal Article)
Sitemtc-m21b.sid.inpe.br
Código do Detentorisadg {BR SPINPE} ibi 8JMKD3MGPCW/3DT298S
Identificador8JMKD3MGP3W34P/3QL77RL
Repositóriosid.inpe.br/mtc-m21b/2018/03.02.14.18   (acesso restrito)
Última Atualização2018:03.02.14.18.54 (UTC) simone
Repositório de Metadadossid.inpe.br/mtc-m21b/2018/03.02.14.18.55
Última Atualização dos Metadados2019:01.14.17.05.24 (UTC) administrator
DOI10.1002/joc.5208
ISSN0899-8418
Rótuloself-archiving-INPE-MCTIC-GOV-BR
Chave de CitaçãoDasariLaViRaPaHo:2018:ENInIn
TítuloENSO influence on the interannual variability of the Red Sea convergence zone and associated rainfall
Ano2018
Data de Acesso16 maio 2024
Tipo de Trabalhojournal article
Tipo SecundárioPRE PI
Número de Arquivos1
Tamanho2101 KiB
2. Contextualização
Autor1 Dasari, Hari Prasad
2 Langodan, Sabique
3 Viswanadhapalli, Yesubabu
4 Rao, Vadlamudi Brahmananda
5 Papadopoulos, Vassilis P.
6 Hoteit, Ibrahim
Identificador de Curriculo1
2
3
4 8JMKD3MGP5W/3C9JJAJ
ORCID1 0000-0003-0628-4481
2 0000-0003-0513-1790
3
4
5
6 0000-0002-3751-4393
Grupo1
2
3
4 CGCPT-CGCPT-INPE-MCTIC-GOV-BR
Afiliação1 King Abdullah University of Science and Technology (KAUST)
2 King Abdullah University of Science and Technology (KAUST)
3 Weather and Climate Research Group, National Atmospheric Research Laboratory
4 Instituto Nacional de Pesquisas Espaciais (INPE)
5 Hellenic Centre for Marine Research
6 King Abdullah University of Science and Technology (KAUST)
RevistaInternational Journal of Climatology
Volume38
Número2
Páginas761-775
Nota SecundáriaA1_GEOCIÊNCIAS A1_ENGENHARIAS_I A1_CIÊNCIAS_AMBIENTAIS A1_CIÊNCIAS_AGRÁRIAS_I A2_INTERDISCIPLINAR A2_BIODIVERSIDADE B1_CIÊNCIAS_BIOLÓGICAS_I
Histórico (UTC)2018-03-02 14:21:12 :: simone -> administrator :: 2018
2018-06-21 01:45:47 :: administrator -> simone :: 2018
2018-06-25 15:51:10 :: simone -> administrator :: 2018
2019-01-04 16:56:02 :: administrator -> simone :: 2018
2019-01-07 14:30:41 :: simone -> administrator :: 2018
2019-01-14 17:05:24 :: 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-ChaveRed Sea convergence zone
Red Sea trough
ENSO
rainfall
moisture convergence
Resumo: The Red Sea convergence zone (RSCZ) is formed by opposite surface winds blowing from northwest to southeast directions at around 18∘ 19∘N between October and January. A reverse-oriented, low-level monsoon trough at 850 hPa, known as the Red Sea trough (RST), transfers moisture from the southern Red Sea to RSCZ. The positions of the RSCZ and RST and the intensity of the RST have been identified as important factors in modulating weather and climatic conditions across the Middle East. Here, we investigate the influence of the El Niño southern oscillation (ENSO) on the interannual variability of RSCZ, RST, and regional rainfall during winter months. Our results indicate that El Niño (warm ENSO phase) favours a shift of the RSCZ to the north and a strengthening of the RST in the same direction. Conversely, during November and December of La Niña periods (cold ENSO phase), the RSCZ shift to the south and the RST strengthens in the same direction. During El Niño periods, southeasterly wind speeds increase (2030%) over the southern Red Sea and northwesterly wind speeds decrease (1015%) over the northern Red Sea. Noticeable increases in the number of rainy days and the intensity of rain events are observed during El Niño phases. These increases are associated with colder than normal air intrusion at lower levels from the north combined with warm air intrusion from the south over the RSCZ. Our analysis suggests that during El Niño winters, warmer sea surface temperatures and higher convective instability over the Red Sea favour local storms conditions and increase rainfall over the Red Sea and adjoining regions.
ÁreaMET
Arranjourlib.net > BDMCI > Fonds > Produção anterior à 2021 > LABAC > ENSO influence on...
Conteúdo da Pasta docacessar
Conteúdo da Pasta sourcenão têm arquivos
Conteúdo da Pasta agreement
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4. Condições de acesso e uso
Idiomaen
Arquivo Alvodasari_enso.compressed.pdf
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simone
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Política de Arquivamentodenypublisher denyfinaldraft
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5. Fontes relacionadas
Unidades Imediatamente Superiores8JMKD3MGPCW/3EUPEJL
Lista de Itens Citandosid.inpe.br/bibdigital/2013/10.06.18.03 4
sid.inpe.br/mtc-m21/2012/07.13.15.01.10 3
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 electronicmailaddress format isbn lineage mark mirrorrepository month nextedition notes parameterlist parentrepositories previousedition previouslowerunit progress project rightsholder schedulinginformation secondarydate secondarykey session shorttitle sponsor subject tertiarymark tertiarytype url
7. Controle da descrição
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1. Identificação
Tipo de ReferênciaArtigo em Revista Científica (Journal Article)
Sitemtc-m16b.sid.inpe.br
Código do Detentorisadg {BR SPINPE} ibi 8JMKD3MGPCW/3DT298S
Identificador6qtX3pFwXQZGivnK2Y/TL9jh
Repositóriosid.inpe.br/mtc-m17@80/2008/04.14.13.59   (acesso restrito)
Última Atualização2008:04.14.13.59.02 (UTC) administrator
Repositório de Metadadossid.inpe.br/mtc-m17@80/2008/04.14.13.59.04
Última Atualização dos Metadados2021:02.10.19.21.45 (UTC) administrator
Chave SecundáriaINPE--PRE/
DOI10.1002/hyp.6813
ISSN0885-6087
Chave de CitaçãoTomasellaHoCuNoWaOl:2007:EfInVa
TítuloThe water balance of an Amazonian micro-catchment: the effect of interannual variability of rainfall on hydrological behaviour
Ano2007
Data Secundária20071104
MêsOct.
Data de Acesso16 maio 2024
Tipo SecundárioPRE PI
Número de Arquivos1
Tamanho1118 KiB
2. Contextualização
Autor1 Tomasella, Javier
2 Hodnett, Martin G.
3 Cuartas, Luz Adriana
4 Nobre, Antonio D.
5 Waterloo, Maarten J.
6 Oliveira, Sylvia M.
Identificador de Curriculo1 8JMKD3MGP5W/3C9JHE3
Grupo1 DOP-INPE-MCT-BR
2
3 CPT-INPE-MCT-BR
Afiliação1 Instituto Nacional de Pesquisas Espaciais (INPE)
2 Department of Hydrology and Geo-environmental Sciences, Faculty of Earth and Life Sciences, Vrije Universiteit, De Boelelaan 1085, 1081 HV Amsterdam, The Netherlands
3 Instituto Nacional de Pesquisas Espaciais (INPE)
4 Instituto Nacional de Pesquisas da Amazônia
5 Department of Hydrology and Geo-environmental Sciences, Faculty of Earth and Life Sciences, Vrije Universiteit, De Boelelaan 1085, 1081 HV Amsterdam, The Netherlands
6 Instituto Nacional de Pesquisas da Amazônia
Endereço de e-Maildeicy@cptec.inpe.br
RevistaHydrological Processes
Volume*
Número*
Páginas*
Histórico (UTC)2009-08-28 21:04:16 :: deicy -> erich@sid.inpe.br ::
2009-08-31 14:35:26 :: erich@sid.inpe.br -> administrator ::
2010-05-11 02:16:30 :: administrator -> erich@sid.inpe.br ::
2010-05-14 02:58:59 :: erich@sid.inpe.br -> administrator ::
2021-02-10 19:21:45 :: administrator -> marciana :: 2007
3. Conteúdo e estrutura
É a matriz ou uma cópia?é a matriz
Estágio do Conteúdoconcluido
Transferível1
Tipo do ConteúdoExternal Contribution
Palavras-Chavewater balance • Amazonian micro-catchment • interannual variability
ResumoIn humid tropical systems, the large intraseasonal and interannual variability of rainfall can significantly affect all components of the water balance. This variability and the lack of detailed hydrological and meteorological data in both temporal and spatial scales have created uncertainties regarding the closure of the water balance for the Amazon basin. Previous studies in Amazonian micro-catchments suggested that both the unsaturated and groundwater system, which are not taken into consideration in basin-wide water budgets published in the literature, play an important role in controlling the timing of runoff generation. In this paper, the components of the water balance and the variations in different storages within the system were examined using 3 years' data from a 6·58 km2 micro-catchment in central Amazonia. The role and relative importance of the various stores were examined. The results show a strong memory effect in the groundwater system that carries over seasonal climate anomalies from one year to the next and affects the hydrological response well beyond the time span of the anomaly. In addition, the deep unsaturated zone was found to play a key role in reducing most of the intraseasonal variability and also affected the groundwater recharge. This memory effect is crucial for sustaining streamflow and evaporation in years with rainfall deficiency. The memory effect caused by storage in the groundwater and unsaturated systems may also prevent the closure of annual large-scale water balances, which assume that storage returns to a standard state each year. Copyright © 2007 John Wiley & Sons, Ltd..
ÁreaMET
Arranjo 1urlib.net > BDMCI > Fonds > Produção anterior à 2021 > CGCPT > The water balance...
Arranjo 2urlib.net > BDMCI > Fonds > Produção anterior à 2021 > DIDOP > The water balance...
Conteúdo da Pasta docacessar
Conteúdo da Pasta sourcenão têm arquivos
Conteúdo da Pasta agreementnão têm arquivos
4. Condições de acesso e uso
Idiomaen
Arquivo AlvoTomasella et al, 2008. the water balanace of an amazonian micr-catchment-1.pdf
Grupo de Usuáriosadministrator
deicy
erich@sid.inpe.br
Visibilidadeshown
Política de Arquivamentodenypublisher denyfinaldraft
Permissão de Leituradeny from all and allow from 150.163
5. Fontes relacionadas
Unidades Imediatamente Superiores8JMKD3MGPCW/3EUPEJL
8JMKD3MGPCW/43SQKNE
DivulgaçãoWEBSCI; PORTALCAPES; MGA; COMPENDEX.
Acervo Hospedeirolcp.inpe.br/ignes/2004/02.12.18.39
cptec.inpe.br/walmeida/2003/04.25.17.12
6. Notas
Campos Vaziosalternatejournal archivist callnumber copyholder copyright creatorhistory descriptionlevel documentstage electronicmailaddress format isbn label lineage mark mirrorrepository nextedition notes orcid parameterlist parentrepositories previousedition previouslowerunit progress project readergroup rightsholder schedulinginformation secondarymark session shorttitle sponsor subject tertiarymark tertiarytype typeofwork url versiontype
7. Controle da descrição
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1. Identificação
Tipo de ReferênciaArtigo em Evento (Conference Proceedings)
Sitemtc-m16d.sid.inpe.br
Código do Detentorisadg {BR SPINPE} ibi 8JMKD3MGPCW/3DT298S
Identificador8JMKD3MGP7W/383L8Q8
Repositóriosid.inpe.br/mtc-m19@80/2010/08.12.19.04
Última Atualização2011:02.09.11.08.06 (UTC) administrator
Repositório de Metadadossid.inpe.br/mtc-m19@80/2010/08.12.19.04.28
Última Atualização dos Metadados2021:01.03.02.14.29 (UTC) administrator
Chave SecundáriaINPE--PRE/
Chave de CitaçãoGiarollaBaetCecc:2010:NDMOSe
TítuloNDVI (MODIS sensor) response to interannual variability of rainfall and evapotranspiration in a soybean producing region, southern Brazil
FormatoOn-line
Ano2010
Data de Acesso16 maio 2024
Tipo SecundárioPRE CI
Número de Arquivos1
Tamanho10 KiB
2. Contextualização
Autor1 Giarolla, Angelica
2 Baethgen, W. E
3 Ceccato, P
Identificador de Curriculo1 8JMKD3MGP5W/3C9JGHP
Grupo1 DSA-CPT-INPE-MCT-BR
Afiliação1 Instituto Nacional de Pesquisas Espaciais (INPE)
2 International Research Institute for Climate and Society (IRI), The Earth Institute, Columbia University, Lamont Campus, Palisades, New York, USA
3 International Research Institute for Climate and Society (IRI), The Earth Institute, Columbia University, Lamont Campus, Palisades, New York, USA
EditorWagner W., Székely, B.
Endereço de e-Mailalessandra@sid.inpe.br
Nome do EventoInternational Society for Photogrammetry and Remote Sensing Symposium, (ISPRS).
Localização do EventoVienna, Austria.
Data5–7July 2010
Volume38 Part 7B
Histórico (UTC)2011-02-09 11:13:09 :: alessandra@sid.inpe.br -> administrator :: 2010
2021-01-03 02:14:29 :: administrator -> alessandra@sid.inpe.br :: 2010
3. Conteúdo e estrutura
É a matriz ou uma cópia?é a matriz
Estágio do Conteúdoconcluido
Transferível1
Tipo do ConteúdoExternal Contribution
Palavras-Chavesoybean (Glycine Max
L. Merr)
NDVI
remote sensing
water balance
GIS
ResumoThis study aimed at evaluating the response of the Normalized Difference Vegetation Index - NDVI (MODIS sensor, TERRA satellite) of soybean to interannual variability of rainfall and evapotranspiration in Campos Gerais, a region of the state of Parana in southern Brazil. Landsat TM 5 and 7 images were selected for analyzing the spatial soybean field distribution for the region from 2000/01 to 2006/07 and to identify soybean fields. We then identified 175 pixels (250 x 250m) that contained only soybean fields (pure-pixels) based on the soybean maps obtained with the Landsat TM images. The next step was to extract the NDVI values for these soybean pure-pixels and to analyze the NDVI spectral curves considering the soybean phenology. Data from nearby meteorological stations were obtained and used to calculate the soil water balance for soybean fields in 5 locations distributed in the Campos Gerais region. To obtain actual evapotranspiration values, the water balance was calculated for each year, and for the same period covering the entire soybean growing season. Anomaly values were calculated for each year to verify the interannual rainfall variability. Linear regression models were adjusted between NDVI and i) rainfall and ii) actual evapotranspiration for all time series. Analysis of the evolution of NDVI values allowed identifying the soybean growing season (November to March) and also the dry season for this region according to rainfall anomaly values. Statistical analyses showed that actual evapotranspiration presented best agreement with soybean NDVI in relation to rainfall, probably due to the fact that this variable integrates information of rainfall, temperature and soil water holding capacity for the entire study period.
ÁreaMET
Arranjourlib.net > Fonds > Produção anterior à 2021 > DIDSA > NDVI (MODIS sensor)...
Conteúdo da Pasta docacessar
Conteúdo da Pasta sourcenão têm arquivos
Conteúdo da Pasta agreementnão têm arquivos
4. Condições de acesso e uso
URL dos dadoshttp://urlib.net/ibi/8JMKD3MGP7W/383L8Q8
URL dos dados zipadoshttp://urlib.net/zip/8JMKD3MGP7W/383L8Q8
Idiomaen
Arquivo AlvoRSAP-135.pdf
Grupo de Usuáriosadministrator
alessandra@sid.inpe.br
Visibilidadeshown
Permissão de Atualizaçãonão transferida
5. Fontes relacionadas
Repositório Espelhosid.inpe.br/mtc-m19@80/2009/08.21.17.02.53
Unidades Imediatamente Superiores8JMKD3MGPCW/43SRC6S
Lista de Itens Citandosid.inpe.br/mtc-m21/2012/07.13.14.40.06 1
sid.inpe.br/bibdigital/2021/01.03.02.10 1
Acervo Hospedeirosid.inpe.br/mtc-m19@80/2009/08.21.17.02
6. Notas
NotasISPRS TC VII Symposium – 100 Years ISPRS
Campos Vaziosarchivingpolicy archivist booktitle callnumber copyholder copyright creatorhistory descriptionlevel dissemination doi edition electronicmailaddress isbn issn label lineage mark nextedition numberofvolumes orcid organization pages parameterlist parentrepositories previousedition previouslowerunit progress project publisher publisheraddress readergroup readpermission rightsholder schedulinginformation secondarydate secondarymark serieseditor session shorttitle sponsor subject tertiarymark tertiarytype type url versiontype
7. Controle da descrição
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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/2005/10.31.22.07
Última Atualização2006:04.15.18.26.00 (UTC) administrator
Repositório de Metadadoscptec.inpe.br/adm_conf/2005/10.31.22.07.44
Última Atualização dos Metadados2018:06.05.03.43.02 (UTC) administrator
Chave de CitaçãoGrimmZill:2006:LaInRo
TítuloInterannual variability of summer rainfall in South America: large-scale influences and the role of antecedent conditions in spring
FormatoCD-ROM, On-line.
Ano2006
Data de Acesso16 maio 2024
Tipo SecundárioPRE CI
Número de Arquivos1
Tamanho633 KiB
2. Contextualização
Autor1 Grimm, Alice Marlene
2 Zilli, Marcia Terezinha
Afiliação1 Universidade Federal do Paraná, Departamento de Física
2 Caixa Postal 19044. 81531-990 Curitiba, PR, Brazil (Grimm
3 Zilli)
Endereço de e-Mail do Autor1 grimm@fisica.ufpr.br
2 marciatz@fisica.ufpr.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
Páginas1097-1103
Título do LivroProceedings
Tipo TerciárioOral
OrganizaçãoAmerican Meteorological Society (AMS)
Histórico (UTC)2005-10-31 22:07:45 :: grimm@fisica.ufpr.br -> adm_conf ::
2005-12-15 15:35:20 :: adm_conf -> grimm@fisica.ufpr.br ::
2006-03-30 00:14:21 :: grimm@fisica.ufpr.br -> administrator ::
2006-04-18 21:17:36 :: administrator -> lise@dpi.inpe.br ::
2010-12-28 12:36:47 :: lise@dpi.inpe.br -> administrator ::
2010-12-29 15:58:48 :: administrator -> lise@dpi.inpe.br :: 2006
2010-12-29 16:06:12 :: lise@dpi.inpe.br -> administrator :: 2006
2010-12-29 18:54:32 :: administrator -> banon :: 2006
2011-01-02 17:15:12 :: banon -> administrator :: 2006
2018-06-05 03:43:02 :: administrator -> :: 2006
3. Conteúdo e estrutura
É a matriz ou uma cópia?é a matriz
Estágio do Conteúdoconcluido
Transferível1
Palavras-ChaveSouth American monsoon system
precipitation
modes of variability
sea surface temperature
land-suface processes
ResumoThe importance of the summer monsoon season to the annual total precipitation over most of South America is well known. The variability of monsoon precipitation is of utmost importance for agriculture, reservoir management, and natural disaster preparedness. Two previous studies with reconstructed rainfall from satellite estimates and gauge-based monthly totals, have stressed the influence of ENSO on summer precipitation. It is represented by the first mode of variability in these studies. The second mode represents the interannual and interdecadal variability in Northeast Brazil, whereas the third mode is completely different in both studies. The first two modes of summer precipitation in those studies do not have strongest components in the monsoon core region in South America. Are the regions with monsoon-like regime not prone to undergo strong interannual variations or, in other words, are the processes leading to monsoon rainfall in South America not prone to undergo interannual variations? If yes, would these processes be directly affected by remote or large-scale influences or indirectly, through regional interactions that are stronger in the summer season? In this study we intend to cast some light on these questions. We pursue the following objectives: i) to determine the principal modes of interannual variability of summer monsoon rainfall on the basis of relatively long series of rain gauge data; ii) to establish connections between the conditions in the beginning of the monsoon season and its peak; iii) to verify connections with global SST. Precipitation data from more than 9000 stations over most of South America are averaged in 2.5 X 2.5 degree boxes. These data are mainly concentrated in the Southern Hemisphere (SH) part of South America, where summer rainfall mostly dominates the annual cycle. Mean precipitation series for spring (SON) and summer (DJF) are formed for each of those boxes in the period 1961-2000, and submitted to Principal Component Analysis. Rotated and non-rotated modes of variability are determined and their relationship with global sea surface temperature SST) is assessed. Furthermore, we analyze the relationship between spring and summer precipitation, in order to detect influence of antecedent soil moisture conditions in spring on the peak summer monsoon rainfall. While some modes of summer rainfall variability bear similarity to modes determined in previous studies, there are also significant differences. There is an inverse relationship between a pair of similar modes in spring and summer, which suggests that antecedent conditions in spring may influence precipitation in summer. This relationship is even stronger when shorter periods within these seasons are analyzed, such as November and January. The analysis of the relationship between the precipitation modes and global SST indicates that the remote large-scale influences on interannual precipitation variability are much stronger in spring than in summer, suggesting a possible role of regional forcing in summer associated with surface-atmosphere interaction..
ÁreaMET
TipoMonsoon systems and continental rainfall
Conteúdo da Pasta docacessar
Conteúdo da Pasta source
ICSHMO_2006_final_VarInteran.doc 29/03/2006 21:14 525.0 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/2005/10.31.22.07
URL dos dados zipadoshttp://mtc-m16b.sid.inpe.br/zip/cptec.inpe.br/adm_conf/2005/10.31.22.07
Idiomaen
Arquivo Alvo1097-1104.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 Revista Científica (Journal Article)
Sitemtc-m21d.sid.inpe.br
Código do Detentorisadg {BR SPINPE} ibi 8JMKD3MGPCW/3DT298S
Identificador8JMKD3MGP3W34T/45DD6DS
Repositóriosid.inpe.br/mtc-m21d/2021/09.09.11.55
Última Atualização2021:09.09.11.55.41 (UTC) simone
Repositório de Metadadossid.inpe.br/mtc-m21d/2021/09.09.11.55.41
Última Atualização dos Metadados2022:04.03.22.27.34 (UTC) administrator
DOI10.3390/atmos12091094
ISSN2073-4433
Chave de CitaçãoKayanoAndrCéroSouz:2021:RoInOc
TítuloThe role of the indian ocean basin-wide and el niño–southern oscillation modes in interannual rainfall variability over south america during austral summer
Ano2021
MêsSept.
Data de Acesso16 maio 2024
Tipo de Trabalhojournal article
Tipo SecundárioPRE PI
Número de Arquivos1
Tamanho7477 KiB
2. Contextualização
Autor1 Kayano, Mary Toshie
2 Andreoli, Rita Valéria
3 Céron, Wilmar L.
4 Souza, Rodrigo A. F.
Identificador de Curriculo1 8JMKD3MGP5W/3C9JHST
ORCID1 0000-0002-2516-295X
2
3 0000-0003-1901-9572
Grupo1 DIMNT-CGCT-INPE-MCTI-GOV-BR
Afiliação1 Instituto Nacional de Pesquisas Espaciais (INPE)
2 Universidade do Estado do Amazonas (UEA)
3 Universidad del Valle
4 Universidade do Estado do Amazonas (UEA)
Endereço de e-Mail do Autor1 mary.kayano@inpe.br
2
3 wilmar.ceron@correounivalle.edu.co
4 rafsouza@uea.edu.br
RevistaAtmosphere
Volume12
Número9
Páginase1094
Nota SecundáriaB3_ENGENHARIAS_III B3_ENGENHARIAS_I B3_CIÊNCIAS_AMBIENTAIS B4_ENGENHARIAS_II B5_GEOCIÊNCIAS
Histórico (UTC)2021-09-09 11:55:41 :: simone -> administrator ::
2021-09-09 11:55:42 :: administrator -> simone :: 2021
2021-09-09 12:00:32 :: simone -> administrator :: 2021
2022-04-03 22:27:34 :: administrator -> simone :: 2021
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-ChaveClimate variability
ENSO
Rainfall
Rossby wave train
South America
Teleconnections
Tropical Indian ocean
ResumoThis paper examines the relative role of the Indian Ocean basin-wide (IOBW) mode and El NiñoSouthern Oscillation (ENSO) in the atmospheric circulation and rainfall interannual variations over South America (SA) during southern summer of the 1951‒2016 period. The effects of the warm IOBW and El Niño (EN) events, and of the cold IOBW and La Niña (LN) events are examined using partial correlations. The ENSO and IOBW modes, through the associated large-scale and regional anomalous circulation patterns, induce contrasting effects on the rainfall in northeastern SA. The EN without the warm IOBW effect induces anomalously dry conditions over eastern Amazon and part of northeastern Brazil (NEB) through anomalous sinking motions of the EN-related anomalous Walker and Hadley cells and strong moisture divergence associated with a vigorous anticyclone over tropical South Atlantic (TSA) and SA. The warm IOBW without the EN effect induces anomalously wet conditions in NEB, which is marginally related to the anomalous Walker and Hadley cells but is modulated by an anticyclone over SA between the equator and 20° S, and a cyclone in the southwestern Atlantic between 20° S and 40° S. The results here might be relevant for climate monitoring and modeling studies.
ÁreaMET
Arranjourlib.net > BDMCI > Fonds > Produção a partir de 2021 > CGCT > The role of...
Conteúdo da Pasta docacessar
Conteúdo da Pasta sourcenão têm arquivos
Conteúdo da Pasta agreement
agreement.html 09/09/2021 08:55 1.0 KiB 
4. Condições de acesso e uso
URL dos dadoshttp://urlib.net/ibi/8JMKD3MGP3W34T/45DD6DS
URL dos dados zipadoshttp://urlib.net/zip/8JMKD3MGP3W34T/45DD6DS
Idiomaen
Arquivo Alvokayano_role.pdf
Grupo de Usuáriossimone
Grupo de Leitoresadministrator
simone
Visibilidadeshown
Política de Arquivamentoallowpublisher allowfinaldraft
Permissão de Atualizaçãonão transferida
5. Fontes relacionadas
Unidades Imediatamente Superiores8JMKD3MGPCW/46KUATE
Lista de Itens Citandosid.inpe.br/bibdigital/2022/04.03.22.23 1
sid.inpe.br/mtc-m21/2012/07.13.14.56.22 1
DivulgaçãoWEBSCI; PORTALCAPES; SCOPUS.
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 mirrorrepository nextedition notes parameterlist parentrepositories previousedition previouslowerunit progress project readpermission rightsholder schedulinginformation secondarydate secondarykey session shorttitle sponsor subject tertiarymark tertiarytype url
7. Controle da descrição
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