Improved snow model captures Northeast's winter thaws and runoff more accurately
Mountain snow in the Northeast is different. The region's milder, more humid mountain climate shapes winter conditions that are different from those of the western United States. Yet, snow models don't always capture those differences.
A new study published in the journal Water Resources Research has improved a snow model to better represent winter conditions in the Northeastern United States. The University of Vermont-led team applied the physics-based model to Mount Mansfield, the highest peak in Vermont's Green Mountain range. The model showed enhanced accuracy in simulating snow water equivalent, depth, density, and melt-driven runoff compared to previous models.
The research highlights the importance of understanding snowpack dynamics in the region, as winters become warmer and wetter. Snowpack is critical to ecosystems and communities, and the study offers valuable insights for flood modeling and forecasting.
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