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 9B
Instantaneous streamflow, suspended-sediment concentrations, and percent sand of suspended sediment during storm events at the Middle Yuba River (11410000) and South Yuba River (11417500) gaging stations in the upper Yuba River watershed, California, December 2002.
Note that the inset in 9B displays suspended-sediment concentration samples collected during the December 2002 storm peak, X’s denote the date and time of samples analyzed for percent sand, and there are no grain-size data from the February 2003 event at Middle Yuba River gage.
Figure 9B - Instantaneous streamflow, suspended-sediment concentrations, and percent sand of suspended sediment during storm events at the Middle Yuba River (11410000) and South Yuba River (11417500) gaging stations in the upper Yuba River watershed, California, December 2002.