Sea-tide effects on flows in the lower reaches of the Amazon River
The physical influence of sea tides on the lower reaches of the Amazon River can be identified more than 1000 km upstream from the sea. Analysis of upstream tidal wave propagation on the Amazon River contributes to the understanding of the hydrodynamics of the lower reaches and to the quantification...
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| Veröffentlicht in: | Hydrological processes 2009-10, Vol.23 (22), p.3141-3150 |
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| container_title | Hydrological processes |
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| creator | Kosuth, Pascal Callède, Jacques Laraque, Alain Filizola, Naziano Guyot, Jean Loup Seyler, Patrick Fritsch, Jean Marie Guimarães, Valdemar |
| description | The physical influence of sea tides on the lower reaches of the Amazon River can be identified more than 1000 km upstream from the sea. Analysis of upstream tidal wave propagation on the Amazon River contributes to the understanding of the hydrodynamics of the lower reaches and to the quantification of the influence of sea level on sedimentation rates. Continuous over-the-year recording of water levels has been undertaken at eight locations along the lower reaches of the Amazon River and flow measurement campaigns have been organized for different river discharge rates (100 000 m³ s⁻¹, 190 000 m³ s⁻¹ and 250 000 m³ s⁻¹) and sea-tide amplitudes (2-3·5 m). Damping, time-delay and deformation of the tidal wave signals, depending on water regimes and distances from the sea, have been analyzed. The physical processes of wave propagation and cyclic water storage and release have been investigated both through data analysis and the application of mathematical hydrodynamic models. The impact of tidal pulses on sediment transport to the sea has been assessed. Copyright © 2009 John Wiley & Sons, Ltd. |
| doi_str_mv | 10.1002/hyp.7387 |
| format | Article |
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Analysis of upstream tidal wave propagation on the Amazon River contributes to the understanding of the hydrodynamics of the lower reaches and to the quantification of the influence of sea level on sedimentation rates. Continuous over-the-year recording of water levels has been undertaken at eight locations along the lower reaches of the Amazon River and flow measurement campaigns have been organized for different river discharge rates (100 000 m³ s⁻¹, 190 000 m³ s⁻¹ and 250 000 m³ s⁻¹) and sea-tide amplitudes (2-3·5 m). Damping, time-delay and deformation of the tidal wave signals, depending on water regimes and distances from the sea, have been analyzed. The physical processes of wave propagation and cyclic water storage and release have been investigated both through data analysis and the application of mathematical hydrodynamic models. The impact of tidal pulses on sediment transport to the sea has been assessed. 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Process</addtitle><description>The physical influence of sea tides on the lower reaches of the Amazon River can be identified more than 1000 km upstream from the sea. Analysis of upstream tidal wave propagation on the Amazon River contributes to the understanding of the hydrodynamics of the lower reaches and to the quantification of the influence of sea level on sedimentation rates. Continuous over-the-year recording of water levels has been undertaken at eight locations along the lower reaches of the Amazon River and flow measurement campaigns have been organized for different river discharge rates (100 000 m³ s⁻¹, 190 000 m³ s⁻¹ and 250 000 m³ s⁻¹) and sea-tide amplitudes (2-3·5 m). Damping, time-delay and deformation of the tidal wave signals, depending on water regimes and distances from the sea, have been analyzed. The physical processes of wave propagation and cyclic water storage and release have been investigated both through data analysis and the application of mathematical hydrodynamic models. The impact of tidal pulses on sediment transport to the sea has been assessed. 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Damping, time-delay and deformation of the tidal wave signals, depending on water regimes and distances from the sea, have been analyzed. The physical processes of wave propagation and cyclic water storage and release have been investigated both through data analysis and the application of mathematical hydrodynamic models. The impact of tidal pulses on sediment transport to the sea has been assessed. Copyright © 2009 John Wiley & Sons, Ltd.</abstract><cop>Chichester, UK</cop><pub>John Wiley & Sons, Ltd</pub><doi>10.1002/hyp.7387</doi><tpages>10</tpages></addata></record> |
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| subjects | Amazon River Brazil Environmental Sciences Freshwater hydrodynamics hydrology mathematical models rivers sea level sediment deposition sediment transport stream flow tidal effects tides |
| title | Sea-tide effects on flows in the lower reaches of the Amazon River |
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