Satellite remote sensing of river inundation area, stage, and discharge: a review

• Published in: Hydrological processes Vol. 11; no. 10; pp. 1427 - 1439
• Main Author: SMITH, LAURENCE C.
• Format: Journal Article Conference Proceeding
• Language: English
• Published: West Sussex John Wiley & Sons, Ltd 01.08.1997
• Subjects: remote sensing; review; river inundation; synthetic aperture radar, Landsat, floods
• ISSN: 0885-6087; 1099-1085
• DOI: 10.1002/(SICI)1099-1085(199708)11:10<1427::AID-HYP473>3.0.CO;2-S

The growing availability of multi‐temporal satellite data has increased opportunities for monitoring large rivers from space. A variety of passive and active sensors operating in the visible and microwave range are currently operating, or planned, which can estimate inundation area and delineate flood boundaries. Radar altimeters show great promise for directly measuring stage variation in large rivers. It also appears to be possible to obtain estimates of river discharge from space, using ground measurements and satellite data to construct empirical curves that relate water surface area to discharge. Extrapolation of these curves to ungauged sites may be possible for the special case of braided rivers. Where clouds, trees and floating vegetation do not obscure the water surface, high‐resolution visible/infrared sensors provide good delineation of inundated areas. Synthetic aperture radar (SAR) sensors can penetrate clouds and can also detect standing water through emergent aquatic plants and forest canopies. However, multiple frequencies and polarizations are required for optimal discrimination of various inundated vegetation cover types. Existing single‐polarization, fixed‐frequency SARs are not sufficient for mapping inundation area in all riverine environments. In the absence of a space‐borne multi‐parameter SAR, a synergistic approach using single‐frequency, fixed‐polarization SAR and visible/infrared data will provide the best results over densely vegetated river floodplains. © 1997 John Wiley & Sons, Ltd.