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

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


Play all audios:


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.


We thank H. Zebker, C. Birkett and J. Ridley for comments on the manuscript. The Cornell Theory Center provided the computer resources necessary for SAR processing. Gamma Remote Sensing


Research and Consulting provided SAR technical advice. This work was supported by NASA.


Institute for Computational Earth System Science, University of California, Santa Barbara, 93106, California, USA


Douglas E. Alsdorf, John M. Melack, Leal A. K. Mertes & Laura L. Hess


Donald Bren School of Environmental Science and Management, University of California, Santa Barbara , 93106, California, USA


Department of Geography, University of California, Santa Barbara, California, 93106, USA


Department of Geography, University of California, Los Angeles, California, 90095 , USA


Anyone you share the following link with will be able to read this content: