A Doppler Radar for Continuous Remote Measurement of River Ice Velocity
Figure 1. The effect of surface roughness on radar backscatter, and defining terms and parameters
Figure 2. The 3-dB beam width of a radar antenna
ERROR ANALYSIS
VELOCITY FROM A DOPPLER FREQUENCY BAND AND A VIDEO RECORD
Figure 6. Example that quantifies the near- and far-edge velocity ratio with the boresight velocity for a specific case, β = 25 and θa = 20
Ice breakup--March 1993
Figure 8. Calculated θa as a function of time for the raw and peak radar data records for the breakup event
Frazil ice run--December 1993
Figure 13. The part of the radar velocity record or breakup with dispersed ice floes in the river
CONCLUSIONS - CR95_210017
Report Ducumentation Page
CR95_21
Figure 1. The effect of surface roughness on radar backscatter, and defining terms and parameters
Figure 2. The 3-dB beam width of a radar antenna
ERROR ANALYSIS
VELOCITY FROM A DOPPLER FREQUENCY BAND AND A VIDEO RECORD
Figure 6. Example that quantifies the near- and far-edge velocity ratio with the boresight velocity for a specific case, β = 25 and θa = 20
Ice breakup--March 1993
Figure 8. Calculated θa as a function of time for the raw and peak radar data records for the breakup event
Frazil ice run--December 1993
Figure 13. The part of the radar velocity record or breakup with dispersed ice floes in the river
CONCLUSIONS - CR95_210017
Report Ducumentation Page
CR95_21
