301-1 Increasing Precipitation and Runoff Over the Last 70 Years, the Winooski River Basin, Vermont

Poster Number 46

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Wednesday, 8 October 2008
George R. Brown Convention Center, Exhibit Hall E

William R. Hackett1, Paul R. Bierman2, Donna M. Rizzo3 and Lance E. Besaw3, (1)Geology, University of Vermont, Burlington, VT
(2)Geology and School of Natural Resources, University of Vermont, Burlington, VT
(3)College of Engineering and Mathematical Sciences, University of Vermont, Burlington, VT
Analysis of more than seventy years (1936 to 2008) of daily discharge and weather data in the 2,704 km2 Winooski River Basin of northern Vermont shows statistically significant increases in both precipitation and river discharge as well as a regular periodicity on a 10-year cycle. We analyzed data from six discharge stations, both on the Winooski River and on its major tributaries, as well as nine weather stations at five locations within the basin.

At all five weather stations average annual precipitation is increasing. At a 95% confidence level, this trend was significant at three of the five locations. Similarly, each of the six discharge stations showed an increasing trend in total annual discharge; half of these were significant at a 95% confidence level. Lowest annual daily flows increased significantly at all stations. In contrast, highest daily discharges for each year increased at some stations while decreasing at others. Inconsistent peak flow trends between stations could be evidence of the factors associated with changing landuse, which affects the way the sub-basins respond to storm events. In addition to the overall trends in the data, a linear spline reveals a ~10-year cyclicity in total annual precipitation and discharge data, which is well correlated with the behavior of the North Atlantic Oscillation (NAO).

The relationship between weather and discharge has also been changing on a monthly scale, with precipitation increasing significantly at three stations during March or April, while the discharge is trending downward during those same months. This trend may be indicative of the changing timing of seasonality. If spring comes earlier on average, the increases in precipitation could be buffered from the river by earlier snowmelt or increased transpiration reducing spring flows.

See more from this Division: General Discipline Sessions
See more from this Session: Hydrogeology (Posters)

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