Department of Civil and Environmental Engineering
University of Washington
Research

Forests and Snow

Intermittent Snow and Process Dynamics

Snow Surface Temperature and Snow Depth in the Tuolumne Watershed

OLYMPEX


Orographic Precipitation

Mapping temperature in complex terrain

Spatial patterns of snow-fed streamflow

Rain vs. Snow

How meadow ecology relates to snow and climate

Intercomparison of Meteorological Forcing Data from Empirical and Mesoscale Model Sources

Silvicliture to maximize snow retention

Remote sensing of radiation to improve snow modeling

Wildflowers and Snow

Associated Research Results:

Interceptometer

Forest Temperature

Teaching Tools

Manipulating forest density and structure to maximize snow retention in maritime mountain basins

Because snowpack accumulation and melt rates depend on forest structure as well as climate, silvicultural manipulation has the potential to increase snow water storage, change the timing of snowmelt, and restore related ecosystem services, such as fish habitat.

Vegetation changes in maritime mountain basins contribute to shifts in snowmelt and streamflow as much as projected climate change. Over the past 80 years, forest harvesting throughout the western U.S. and western British Columbia has resulted in a shift in the dominant forest structure to young, dense forests. Declining trends in mountain snow water equivalent (SWE), summer river flow, and earlier snowmelt have largely been attributed to climate with little consideration of the role vegetation plays in these hydrologic processes.

Working with Jim Lutz, UW Dept. of Forestry, and Rolf Geronde, Seattle Public Utilities, we are focusing our study on the Cedar River Municipal Watershed (CRMW), located in western Washington, which provides water to more than 1.4 million people and also supports a significant anadromous fishery. The watershed is located in the intermittent snow zone, where the snowpack is most sensitive to climate change. While overall snow accumulation is important, we are primarily concerned with snowmelt timing, since it is crucial to watershed management in basins with limited reservoir storage, as is the case in most of the Pacific Northwest. Any delay in snowmelt from silvicultural manipulation could reduce winter flood hazards and increase summer runoff when water demand for cities, agriculture, and stream ecology is the highest.

Using a combination of distributed field measurements, combined with point and distributed hydrologic models, we propose to address three major questions:

  • 1) What is the variability of snow interception and melt in different forest structures and classes?
  • 2) Over multiple decades, which forest changes are of comparable magnitude to climate change in their effects on snow water storage? Which forest changes exacerbate earlier runoff, and which retain snow longer on the landscape?
  • 3) How can silvicultural practices be used in watershed management to help offset the effects of projected climate change?
  • Material contained here and within the embedded links is based upon work supported by the National Science Foundation under Grant No. 0931780. Any opinions, findings and conclusions or recomendations expressed in this material are those of the author(s) and do not necessarily reflect the views of the National Science Foundation (NSF).