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| Registros recuperados : 16 | |
| 2. |  | IVORY, S.; MCGLUE, M. M.; SPERA, S. A; SILVA, A; BERGIER, I. Disentangling local and regional climatic controls on vegetation and the flood pulse in the Pantanal, the world's largest tropical wetland. In: FALL MEETING, 2018, Washington, D.C. Abstracts... Washington, D.C: American Geophysical Union, 2018. AGU 2018. Session PP23D-1524.| Biblioteca(s): Embrapa Pantanal. |
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| 3. | | McGLUE, M. M.; GUERREIRO, R. L.; BERGIER, I.; SILVA, A.; PUPIM, F. N. Holocene stratigraphic evolution of saline lakes in Nhecolândia, southern Pantanal wetlands (Brazil). Quaternary Research, v. 88, n. 3, p. 472-490, nov. 2017.| Biblioteca(s): Embrapa Pantanal. |
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| 5. | | LO, E. L.; YEAGER, K, M.; BERGIER, I.; DOMINGOS-LUZ, L.; SILVA, A.; MCGLUE, M. M. Sediment infill of tropical floodplain lakes: rates, controls, and implications for ecosystem services. Frontiers in Earth Science, v. 10, 875919, May 2022.| Biblioteca(s): Embrapa Agricultura Digital; Embrapa Pantanal. |
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| 6. | | RASBOLD, G. G.; McGLUE, M. M.; STEVAUX, J. C.; PAROLIN, M.; SILVA, A.; BERGIER, I. Sponge spicule and phytolith evidence for Late Quaternary environmental changes in the tropical Pantanal wetlands of western Brazil. Palaeogeography, Palaeoclimatology, Palaeoecology, v. 518, p. 119-133, 2019.| Biblioteca(s): Embrapa Pantanal. |
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| 7. | | IVORY, S. I.; McGLUE, M. M.; SPERA, S.; SILVA, A.; BERGIER, I. Vegetation, rainfall, and pulsing hydrology in the Pantanal, the world's largest tropical wetland. Environmental Research Letters, v. 14, n. 12, p. 1-11, 2019.| Biblioteca(s): Embrapa Pantanal. |
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| 8. | | BERGIER, I.; ASSINE, M. L.; MCGLUE, M. M.; ALHO, C. J. R.; SILVA, A.; GUERREIRO, R. L.; CARVALHO, J. C. Amazon rainforest modulation of water security in the Pantanal wetland. Science of the Total Environment, v. 619 - 620, p. 1116-1125, apr. 2018.| Biblioteca(s): Embrapa Pantanal. |
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| 10. | | RASBOLD, G. G.; MCGLUE, M. M.; STEVAUX, J. C.; PAROLIN, M.; SILVA, A.; BERGIER, I.; LUZ, L. D. Microfossil and stratigraphic evidence for late quaternary paleoenvironmental changes at Lagoa Negra, Central Pantanal wetlands (Brazil). In: FALL MEETING, 2018, Washington, D.C. Abstracts... Washington, D.C: American Geophysical Union, 2018. Não paginado. AGU 2018. Session PP23D-1525.| Biblioteca(s): Embrapa Pantanal. |
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| 11. | | LOUZADA, R. O.; BERGIER, I.; MCGLUE, M. M.; ROQUE, F. de O.; RASBOLD, G.; DOMINGOS-LUZ, L.; LO, E.; ASSINE, M. L. Fluvial avulsions influence soil fertility in the Pantanal wetlands (Brazil). Science of the Total Environment, v. 926, 172127, May 2024.| Biblioteca(s): Embrapa Agricultura Digital. |
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| 12. | | Lo, E. L.; McGLUE, M. M.; SILVA, A.; BERGIER, I.; YEAGER, K. M.; MACEDO, H. DE.; SWALLOMA, M.; ASSINE, M. L. Fluvio-lacustrine sedimentary processes and landforms on the distal Paraguay fluvial megafan (Brazil). Geomorphology, v. 342, p. 163-175, 2019.| Biblioteca(s): Embrapa Pantanal. |
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| 13. | | GUERREIRO, R. L.; MCGLUE, M. M.; STONE, J. R.; BERGIER, I.; PAROLIN, M.; CAMINHA, S. A. F. da S.; WARREN, L. V.; ASSINE, M. L. Paleoecology explains Holocene chemical changes in lakes of the Nhecolândia (Pantanal-Brazil). Hydrobiologia, v. 815, n. 1, p. 1-19, jun. 2018.| Biblioteca(s): Embrapa Pantanal. |
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| 14. | | GUERREIRO, R. L.; BERGIER, I.; McGLUE, M. M.; WARREN, L. V.; ABREU, U. G. P. de; ABRAHÃO, J.; ASSINE, M. L. The soda lakes of Nhecolândia: a conservation opportunity for the Pantanal wetlands. Perspectives in Ecology and Conservation, v. 17, p. 9-18, 2019.| Biblioteca(s): Embrapa Pantanal. |
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| 15. | | LO, E. L.; SILVA, A.; BERGIER, I.; MCGLUE, M. M.; SILVA, B. L. de; SILVA, A. P. S.; PEREIRA, L. E. P.; MACEDO, H. de A.; ASSINE, M. L.; SILVA, E. R. dos S. da. Papel das macrófitas aquáticas na sucessão ecológica em sistemas fluvio-lacustres do Pantanal: Lago Uberaba. In: SIMPÓSIO DE GEOTECNOLOGIAS NO PANTANAL, 6., 2016, Cuiabá, MT. Anais... São José dos Campos: INPE, 2016. p. 224-233.| Biblioteca(s): Embrapa Pantanal. |
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| 16. | | LO, E. L.; SILVA, A.; BERGIER, I.; MCGLUE, M. M.; SILVA, B. L. de P.; SILVA, A. P. S.; PEREIRA, L. E.; MACEDO, H. de A.; ASSINE, M. L.; SILVA, E. R. dos S. da. Spatiotemporal evolution of the margins of lake Uberaba, Pantanal Floodplain (Brazil). GEOGRAFIA, Rio Claro, v. 42, n. 3, p. 159-173, set./dez. 2017. Especial - GeoPantanal 6.| Biblioteca(s): Embrapa Pantanal. |
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| Registros recuperados : 16 | |
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Registro Completo
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Biblioteca(s): |
Embrapa Pantanal. |
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Data corrente: |
13/12/2019 |
|
Data da última atualização: |
17/02/2022 |
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Tipo da produção científica: |
Artigo em Periódico Indexado |
|
Circulação/Nível: |
A - 1 |
|
Autoria: |
IVORY, S. I.; McGLUE, M. M.; SPERA, S.; SILVA, A.; BERGIER, I. |
|
Afiliação: |
SARAH J IVORY, UNIVERSITY PARK; MICHAEL M McGLUE, UNIVERSITY OF KENTUCKY; STEPHANIE SPERA, UNIVERSITY OF RICHMOND; AGUINALDO SILVA, UFMS; IVAN BERGIER TAVARES DE LIMA, CPAP. |
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Título: |
Vegetation, rainfall, and pulsing hydrology in the Pantanal, the world's largest tropical wetland. |
|
Ano de publicação: |
2019 |
|
Fonte/Imprenta: |
Environmental Research Letters, v. 14, n. 12, p. 1-11, 2019. |
|
DOI: |
10.1088/1748-9326/ab4ffe |
|
Idioma: |
Inglês |
|
Conteúdo: |
Wetlands provide valuable ecosystem services and play a central role in global carbon cycling. Changes in rainfall and the flood-pulse are likely to disrupt the processes that maintain these landscapes; further, landscape modification may dramatically alter wetlands and promote terrestrialization. The Pantanal, South America, is the world?s largest wetland due to flooding along the Upper Paraguay River. Predicting how water resources in the Pantanal may change is problematic due to a complex drainage network, resulting in the out-of-phase timing of rainfall and the flood pulse.Weuse remote sensing data of vegetation and climate to better understand the relationships among the rains, the flood pulse, and vegetation. Although rainfall is regionally synchronous, vegetation responses differ based on position relative to inundated areas. Away from rivers, vegetation greening occurs immediately following rainfall. Along channels, greening may lag rainfall by six months, responding closely to local flood stage. Interannual rainfall variability also impacts vegetation differently near flooded areas, with weaker, lagged responses to rainfall due to local water storage. This work suggests that the importance of flood pulse timing for vegetation productivity in inundated areas means that local conditions in wetlands may be the strongest controls on biogeochemical processes. |
|
Palavras-Chave: |
Ecohydrology. |
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Thesagro: |
Hidrologia; Inundação; Mudança Climática. |
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Thesaurus NAL: |
Climate change; Floods; Pantanal; Wetlands. |
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Categoria do assunto: |
P Recursos Naturais, Ciências Ambientais e da Terra |
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URL: |
https://ainfo.cnptia.embrapa.br/digital/bitstream/item/207009/1/Vegetation-rainfall-and-pulsing-hydrology-2019.pdf
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Marc: |
LEADER 02169naa a2200277 a 4500
001 2116851
005 2022-02-17
008 2019 bl uuuu u00u1 u #d
024 7 $a10.1088/1748-9326/ab4ffe$2DOI
100 1 $aIVORY, S. I.
245 $aVegetation, rainfall, and pulsing hydrology in the Pantanal, the world's largest tropical wetland.$h[electronic resource]
260 $c2019
520 $aWetlands provide valuable ecosystem services and play a central role in global carbon cycling. Changes in rainfall and the flood-pulse are likely to disrupt the processes that maintain these landscapes; further, landscape modification may dramatically alter wetlands and promote terrestrialization. The Pantanal, South America, is the world?s largest wetland due to flooding along the Upper Paraguay River. Predicting how water resources in the Pantanal may change is problematic due to a complex drainage network, resulting in the out-of-phase timing of rainfall and the flood pulse.Weuse remote sensing data of vegetation and climate to better understand the relationships among the rains, the flood pulse, and vegetation. Although rainfall is regionally synchronous, vegetation responses differ based on position relative to inundated areas. Away from rivers, vegetation greening occurs immediately following rainfall. Along channels, greening may lag rainfall by six months, responding closely to local flood stage. Interannual rainfall variability also impacts vegetation differently near flooded areas, with weaker, lagged responses to rainfall due to local water storage. This work suggests that the importance of flood pulse timing for vegetation productivity in inundated areas means that local conditions in wetlands may be the strongest controls on biogeochemical processes.
650 $aClimate change
650 $aFloods
650 $aPantanal
650 $aWetlands
650 $aHidrologia
650 $aInundação
650 $aMudança Climática
653 $aEcohydrology
700 1 $aMcGLUE, M. M.
700 1 $aSPERA, S.
700 1 $aSILVA, A.
700 1 $aBERGIER, I.
773 $tEnvironmental Research Letters$gv. 14, n. 12, p. 1-11, 2019.
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Embrapa Pantanal (CPAP) |
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