Using Altimetry Waveform Data and Ancillary Information from SRTM and LANDSAT to retrieve River Characteristics
Vivien Enjolras(1) and Ernesto RODRIGUEZ(2)
18, av. Edouard Belin,
(2) Jet Propulsion Laboratory, 4800 Oak Grove Drive, PASADENA CA 91109, United States
Spaceborne radar altimeters are shown to have the potential for monitoring the height of large rivers with accuracies of approximately 1 m. However, the need for a better height accuracy and the observations of smaller continental basins have led to studies on how to improve and extend the use of nadir altimeter data.
Conventional retracking techniques over land are limited to the examination of altimeter waveforms on a case by case basis. Due to the arbitrary geometry which may be present at altimeter river crossings, this approach may be limited to large rivers, which approximate ocean crossings.
To overcome this limitation, we introduce a waveform fitting method which uses the entire set of waveforms associated with a water crossing, rather than individual waveforms. By using ancillary data, such as a digital elevation model (obtained from SRTM) and classification maps (obtained from Landsat), it is possible to recast the retracking problems as a maximum likelihood estimation problem. Theoretical power returns based on the a priori knowledge of the observed scenes are generated resulting in a parametric library of waveform histories, which is then used to constrain the estimation. For demonstration, we concentrate on the river Meuse in Northern Western Europe. This river has important social impact, since it has flooded in the past and better real time predictions of its changing stage may improve flood forecasting skill. Furthermore, it presents a challenge to conventional nadir altimeter waveform retracking. We will present both theoretical performance results and demonstrate the feasibility based on real altimeter data.
Keywords: altimetry, waveform, hydrology, Europe