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Why can winter snowfall for some locations vary so much from year to year? This project seeks to explore the relationship between interannual variability of seasonal snowfall in the Northeastern United States and the location of the Gulf Stream in the Atlantic Ocean. Along the northern edge of the Gulf Stream, a strong near-surface air temperature gradient exists with the sharp boundary separating warmer water to the south and cooler water to the north. This temperature gradient serves as the principal energy source for extratropical cyclones, which suggests that its location may have an eff ect on snowfall patterns in the region. We hypothesize that northward shifts in the Gulf Stream cause a corresponding northward shift in snowfall patterns.

Covariation of Snowfall Patterns in the Northeastern United States with the Location of the Gulf Stream