Interferometric radar measurements of water level changes on the Amazon flood plain

Douglas E. Alsdorf (), John M. Melack, Thomas Dunne, Leal A. K. Mertes, Laura L. Hess and Laurence C. Smith
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Douglas E. Alsdorf: Institute for Computational Earth System Science, University of California
John M. Melack: Institute for Computational Earth System Science, University of California
Thomas Dunne: Donald Bren School of Environmental Science and Management, University of California
Leal A. K. Mertes: Institute for Computational Earth System Science, University of California
Laura L. Hess: Institute for Computational Earth System Science, University of California
Laurence C. Smith: University of California

Nature, 2000, vol. 404, issue 6774, 174-177

Abstract: Abstract Measurements of water levels in the main channels of rivers, upland tributaries and floodplain lakes are necessary for understanding flooding hazards, methane production, sediment transport and nutrient exchange. But most remote river basins have only a few gauging stations and these tend to be restricted to large river channels. Although radar remote sensing techniques using interferometric phase measurements have the potential to greatly improve spatial sampling, the phase is temporally incoherent over open water and has therefore not been used to determine water levels. Here we use interferometric synthetic aperture radar (SAR) data1,2,3, acquired over the central Amazon by the Space Shuttle imaging radar mission4, to measure subtle water level changes in an area of flooded vegetation on the Amazon flood plain. The technique makes use of the fact that flooded forests and floodplain lakes with emergent shrubs permit radar double-bounce returns from water and vegetation surfaces5,6, thus allowing coherence to be maintained. Our interferometric phase observations show decreases in water levels of 7–11 cm per day for tributaries and lakes within ∼20 km of a main channel and 2–5 cm per day at distances of ∼80 km. Proximal floodplain observations are in close agreement with main-channel gauge records, indicating a rapid response of the flood plain to decreases in river stage. With additional data from future satellite missions, the technique described here should provide direct observations important for understanding flood dynamics and hydrologic exchange between rivers and flood plains.

Date: 2000
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DOI: 10.1038/35004560

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