A Norwegian/Canadian team developed now an innovative method to measure for the first time ever the complete surface water velocity field over entire river reaches. They use river ice debris as an index of surface water velocity, and track it over a time period of about one minute, which is the typical time lag between the two or more images that form a stereo data set in spaceborne, alongtrack optical stereo mapping. In this way, they measure and visualize for the first time, the almost complete surface velocity field of a river. Examples are used from approximately 80 km and 40 km long reaches of the St. Lawrence and Mackenzie rivers, Canada, respectively, based on ALOS PRISM, ASTER, and IKONOS stereo data.
The methodology and results will be valuable to a number of disciplines requiring detailed information about river flow, such as hydraulics, hydrology, river ecology and natural hazard management.
The result has been presented in the paper A?Â?Cold-regions river flow observed from spaceA?Â? authored by A. KAÂ¤AÂ¤b and T. Prowse, and published on 20 April 2011 on Geophysical Research Letters