Use of Sediment Rating Curves and Optical Backscatter Data to Characterize Sediment Transport in the Upper Yuba River Watershed, California, 2001–03
By Jennifer A. Curtis1, Lorraine E. Flint1, Charles N. Alpers1, Scott A. Wright2 and Noah P. Snyder3
U.S. Geological Survey Scientific Investigations Report  2005–5246 , published 2006.
Figure 11A
Non-linear regression relations between suspended-sediment concentration and instantaneous streamflow for the Middle Yuba River (11410000) and South Yuba River (11417500) gaging stations in the upper Yuba River watershed, California. Average.
See table 4 for regression equation form and summary statistics.
Figure 11A - Non-linear regression relations between suspended-sediment concentration and instantaneous streamflow for the Middle Yuba River (11410000) and South Yuba River (11417500) gaging stations in the upper Yuba River watershed, California. Average.