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Registro Completo |
Biblioteca(s): |
Embrapa Amazônia Oriental. |
Data corrente: |
31/03/2009 |
Data da última atualização: |
22/11/2022 |
Tipo da produção científica: |
Artigo em Periódico Indexado |
Autoria: |
FITZJARRALD, D. R.; SAKAI, K. R.; MORAES, O. L. L.; OLIVEIRA JUNIOR, R. C. de; ACEVEDO, O. C.; CZIKOWSKY, M. J.; BELDINI, T. |
Afiliação: |
David R. Fitzjarrald, Atmospheric Sciences Research Center State University of New York at Albany Albany New York USA; Ricardo K. Sakai, Atmospheric Sciences Research Center State University of New York at Albany, Albany, New York; Osvaldo L. L. Moraes, Departamento de Física Universidade Federal de Santa Maria; RAIMUNDO COSME DE OLIVEIRA JUNIOR, CPATU; Otávio C. Acevedo, Departamento de Física Universidade Federal de Santa Maria, Santa Maria; Matthew J. Czikowsky, Atmospheric Sciences Research Center State University of New York at Albany, Albany, New York; Troy Beldini, Projeto LBA Escritório e Laboratório de Apoio em Santarém, Santarém. |
Título: |
Spatial and temporal rainfall variability near the Amazon-Tapajós confluence. |
Ano de publicação: |
2008 |
Fonte/Imprenta: |
Journal of Geophysical Research: Biogeosciences, v. 113, n. G1, 2008. |
Páginas: |
p. 1-17. |
DOI: |
10.1029/2007JG000596 |
Idioma: |
Inglês |
Conteúdo: |
Do the influences of river breezes or other mesoscale effects lead to a systematic river proximity bias in Amazon rainfall data? We analyzed rainfall for a network of 38 rain gauges located near the confluence of the Tapajós and Amazon rivers in the eastern Amazon Basin. Tipping bucket rain gauges worked adequately in the Amazon rainfall regime, but careful field calibration and comparison with collocated conventional rain gauges were essential to incorporate daily totals from our array into regional maps. Stations very near the large rivers miss the afternoon convective rain, as expected if a river breeze promotes subsidence over the river, but paradoxically, this deficiency is more than compensated by additional nocturnal rainfall at these locations. The NOAA Climate Prediction Center (CPC) Morphing technique (CMORPH) passive infrared inferred rainfall data do an adequate job of describing medium scale variability in this region, but some localized breeze effects are not resolved at 0.25° resolution. For areas inland from the rivers, nocturnal rainfall contributes less than half of total precipitation. A large-scale rainfall increase just to the west of Santarém manifests itself locally as a ?tongue? of enhanced rain from along the wide area of open water at the Tapajós-Amazon confluence. The Amazon River breeze circulation affects rainfall more than does the Tapajós breeze, which moves contrary to the predominant wind. East of the riverbank, the effects of the Tapajós breeze extend only a few kilometers inland. Rainfall increases to the north of the Amazon, possibly the result of uplift over elevated terrain. Dry season rainfall increases by up to 30% going away from the Amazon River, as would be expected given breeze-induced subsidence over the river. MenosDo the influences of river breezes or other mesoscale effects lead to a systematic river proximity bias in Amazon rainfall data? We analyzed rainfall for a network of 38 rain gauges located near the confluence of the Tapajós and Amazon rivers in the eastern Amazon Basin. Tipping bucket rain gauges worked adequately in the Amazon rainfall regime, but careful field calibration and comparison with collocated conventional rain gauges were essential to incorporate daily totals from our array into regional maps. Stations very near the large rivers miss the afternoon convective rain, as expected if a river breeze promotes subsidence over the river, but paradoxically, this deficiency is more than compensated by additional nocturnal rainfall at these locations. The NOAA Climate Prediction Center (CPC) Morphing technique (CMORPH) passive infrared inferred rainfall data do an adequate job of describing medium scale variability in this region, but some localized breeze effects are not resolved at 0.25° resolution. For areas inland from the rivers, nocturnal rainfall contributes less than half of total precipitation. A large-scale rainfall increase just to the west of Santarém manifests itself locally as a ?tongue? of enhanced rain from along the wide area of open water at the Tapajós-Amazon confluence. The Amazon River breeze circulation affects rainfall more than does the Tapajós breeze, which moves contrary to the predominant wind. East of the riverbank, the effects of the Tapajós bre... Mostrar Tudo |
Palavras-Chave: |
Brasil; Tapajós. |
Thesagro: |
Águas Interiores; Bacia Hidrográfica; Balanço Hídrico; Clima; Evaporação; Precipitação Pluvial; Temperatura. |
Thesaurus Nal: |
Amazonia. |
Categoria do assunto: |
P Recursos Naturais, Ciências Ambientais e da Terra |
Marc: |
LEADER 02748naa a2200337 a 4500 001 1410232 005 2022-11-22 008 2008 bl uuuu u00u1 u #d 024 7 $a10.1029/2007JG000596$2DOI 100 1 $aFITZJARRALD, D. R. 245 $aSpatial and temporal rainfall variability near the Amazon-Tapajós confluence.$h[electronic resource] 260 $c2008 300 $ap. 1-17. 520 $aDo the influences of river breezes or other mesoscale effects lead to a systematic river proximity bias in Amazon rainfall data? We analyzed rainfall for a network of 38 rain gauges located near the confluence of the Tapajós and Amazon rivers in the eastern Amazon Basin. Tipping bucket rain gauges worked adequately in the Amazon rainfall regime, but careful field calibration and comparison with collocated conventional rain gauges were essential to incorporate daily totals from our array into regional maps. Stations very near the large rivers miss the afternoon convective rain, as expected if a river breeze promotes subsidence over the river, but paradoxically, this deficiency is more than compensated by additional nocturnal rainfall at these locations. The NOAA Climate Prediction Center (CPC) Morphing technique (CMORPH) passive infrared inferred rainfall data do an adequate job of describing medium scale variability in this region, but some localized breeze effects are not resolved at 0.25° resolution. For areas inland from the rivers, nocturnal rainfall contributes less than half of total precipitation. A large-scale rainfall increase just to the west of Santarém manifests itself locally as a ?tongue? of enhanced rain from along the wide area of open water at the Tapajós-Amazon confluence. The Amazon River breeze circulation affects rainfall more than does the Tapajós breeze, which moves contrary to the predominant wind. East of the riverbank, the effects of the Tapajós breeze extend only a few kilometers inland. Rainfall increases to the north of the Amazon, possibly the result of uplift over elevated terrain. Dry season rainfall increases by up to 30% going away from the Amazon River, as would be expected given breeze-induced subsidence over the river. 650 $aAmazonia 650 $aÁguas Interiores 650 $aBacia Hidrográfica 650 $aBalanço Hídrico 650 $aClima 650 $aEvaporação 650 $aPrecipitação Pluvial 650 $aTemperatura 653 $aBrasil 653 $aTapajós 700 1 $aSAKAI, K. R. 700 1 $aMORAES, O. L. L. 700 1 $aOLIVEIRA JUNIOR, R. C. de 700 1 $aACEVEDO, O. C. 700 1 $aCZIKOWSKY, M. J. 700 1 $aBELDINI, T. 773 $tJournal of Geophysical Research: Biogeosciences$gv. 113, n. G1, 2008.
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Embrapa Amazônia Oriental (CPATU) |
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Biblioteca(s): |
Embrapa Soja. |
Data corrente: |
06/05/1992 |
Data da última atualização: |
13/12/2011 |
Autoria: |
SILVA, C. M. da; MESQUITA, A. N. de; PEREIRA, L. A. G. |
Título: |
Efeito da epoca da colheita na qualidade da semente de soja. |
Ano de publicação: |
1979 |
Fonte/Imprenta: |
Revista Brasileira de Sementes, Brasilia, v.1, n.2, p.41-48, 1979. |
Idioma: |
Português |
Conteúdo: |
Para se determinar a epoca ideal da colheita de semente de soja (Glycine max (L.) Merrill), foram conduzidos experimenos com as cultivares Bossier e Davis. As colheitas para as duas cultivares foram efetuadas naturalmente em quatro epocas diferentes, com um tratamento adicional, colhido a maquina. para a cultivar Davis, as colheitas foram efetuadas de sete em sete dias, a partir de 15% de umidade e, a colheita a maquina, coincidiu com a segunda epoca de colheita manual. Em ambos os experimentos foi determinada a germinacao, mes a mes, e, apos o periodo de armazenagem, as sementes foram submetidas a avaliacao do vigor e potencial germinativo pelo teste de tretrazolio. A cultivar Davis apresenta baixa germinacao, em todas as epocas de colheita. A cultivar Bossier apresentou melhor qualidade de sementes nas primeiras e segunda epocas. |
Palavras-Chave: |
Harvesting time; Quality; Seed; Soybean; Vigour. |
Thesagro: |
Armazenamento; Colheita; Germinação; Glycine Max; Qualidade; Semente; Soja. |
Thesaurus NAL: |
germination; storage; vigor. |
Categoria do assunto: |
-- |
URL: |
https://ainfo.cnptia.embrapa.br/digital/bitstream/item/50135/1/ABRATES13.PDF
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Marc: |
LEADER 01645naa a2200325 a 4500 001 1444746 005 2011-12-13 008 1979 bl uuuu u00u1 u #d 100 1 $aSILVA, C. M. da 245 $aEfeito da epoca da colheita na qualidade da semente de soja. 260 $c1979 520 $aPara se determinar a epoca ideal da colheita de semente de soja (Glycine max (L.) Merrill), foram conduzidos experimenos com as cultivares Bossier e Davis. As colheitas para as duas cultivares foram efetuadas naturalmente em quatro epocas diferentes, com um tratamento adicional, colhido a maquina. para a cultivar Davis, as colheitas foram efetuadas de sete em sete dias, a partir de 15% de umidade e, a colheita a maquina, coincidiu com a segunda epoca de colheita manual. Em ambos os experimentos foi determinada a germinacao, mes a mes, e, apos o periodo de armazenagem, as sementes foram submetidas a avaliacao do vigor e potencial germinativo pelo teste de tretrazolio. A cultivar Davis apresenta baixa germinacao, em todas as epocas de colheita. A cultivar Bossier apresentou melhor qualidade de sementes nas primeiras e segunda epocas. 650 $agermination 650 $astorage 650 $avigor 650 $aArmazenamento 650 $aColheita 650 $aGerminação 650 $aGlycine Max 650 $aQualidade 650 $aSemente 650 $aSoja 653 $aHarvesting time 653 $aQuality 653 $aSeed 653 $aSoybean 653 $aVigour 700 1 $aMESQUITA, A. N. de 700 1 $aPEREIRA, L. A. G. 773 $tRevista Brasileira de Sementes, Brasilia$gv.1, n.2, p.41-48, 1979.
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