Seasat I scatterometer data collected over the Beaufort Sea are analyzed an
d compared with a simple theoretical model that includes surface roughness
and volume scattering. The values of the root-mean-square (rms) surface slo
pe of roughness and the volume scattering albedo are adjusted to fit the da
ta. With qualifications imposed on the theoretical assumptions, the data ar
e well modeled by the tno parameters and the sensor offers a physically bas
ed means to monitor the statistical properties of sea ice using satellite s
catterometers, such as the European Remote Sensing Satellite (ERS-1) and th
e NSCAT, which collected data from the Japanese ADEOS I spacecraft.