High river temperatures have been linked to pre-spawning mortalities i
n salmon returning to their natal streams. As a first step in predicti
ng these temperatures, flow, and temperature models were developed for
the Fraser and Thompson Rivers in British Columbia. The flow model is
essentially pre-calibrated while the temperature model was calibrated
against data collected in 1993 and then verified against data from 19
94. Root mean square differences between measured and calculated tempe
ratures were found to be 0.70 degrees C at thirteen stations in 1993 a
nd 0.60 degrees C at fifteen stations in 1994. As a purely speculative
exercise, the models were then used to investigate the feasibility of
using cooler waters from lakes to reduce the warm temperatures record
ed in 1994.