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Quantifying the restoration success of wood introductions to increase coho salmon winter habitat

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Figure

Table 1. Characteristics of the three study sites. Values in parenthe-sis correspond to the standard errors.
Figure 2. Topography (derived 0.2 m contours) and location of introduced large wood (LW), water surface elevation (WSE) monitoringrulers (circles), water level loggers (triangle), and location of velocity measurements (dash line)
Table 2. Nays2DH model parameters and calibration results for pre- and post-large-wood (LW) models for different discharge (Qi) levels.Fractional bankfull discharge (Qi/Qbf), average model depth (Hmean), number of water surface elevation (WSE) and velocity (v) observa-tions taken, root mean square error (RMSE), R2 for WSE, and time-averaged v are indicated for calibration runs when available along withobserved and modeled WSE slopes.
Table 3. Mean and standard deviation (SD) of velocity (v) and shear stress (τ) at bankfull flow (Qbf) pre- and post-LW at the three studysites; Qbf modeling results for habitat metrics v and τ expressed as a percentage of the channel bed pre- and post-LW; and percentage changein available fish habitat.
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