Some aspects of the hydroclimatology of the Quesnel River Basin, British Columbia, Canada

In conjunction with available climate data, surface runoff is investigated at 12 gauges in the Quesnel watershed of British Columbia to develop its long-term (1926-2004) hydroclimatology. At Quesnel itself, annual mean values of air temperature, precipitation and runoff are 4-6 degrees C, 517 and 648 mm, respectively. Climate data reveal increases in precipitation, no significant trend in mean annual air temperature, but an increasing trend in mean minimum temperatures that is greatest in winter. There is some evidence of decreases in winter snow depth. On the water year scale (October - September), a strong positive correlation is found between discharge and precipitation (r = 0.70, p < 0.01) and a weak negative correlation is found between precipitation and temperature (r = -0-36, p < 0.01). Long-term trends using the Mann-Kendall test indicate increasing annual discharge amounts that vary from 8 to 14% (12% for the Quesnel River, p = 0.03), and also a tendency toward an earlier spring freshet. River runoff increases at a rate of 1.26 mm yr(-1) m(-1) of elevation from west to east along the strong elevation gradient in the basin. Discharge, temperature and precipitation are correlated with the large-scale climate indices of the Pacific Decadal Oscillation (PDO) and El-Nino Southern Oscillation (ENSO). Copyright (C) 2009 John Wiley & Sons, Ltd.