The National Oceanic and Atmospheric Administration/Cooperative Institute for Research in Environmental Sciences Twentieth Century Reanalysis (20CR) is used to explore the feasibility of high-resolution simulation of a historic extratropical cyclone event: The New England Blizzard of 1888. Using the 20CR as initial and lateral boundary conditions for the Weather Research and Forecasting model, a reasonable depiction of the cyclone is obtained, albeit displaced significantly to the north of the observed cyclone during the later stages of the event. Despite the position error, the simulated storm produces heavy snowfall over parts of New England and intense offshore cyclogenesis. © 2013. American Geophysical Union. All Rights Reserved.
CITATION STYLE
Michaelis, A. C., & Lackmann, G. M. (2013). Numerical modeling of a historic storm: Simulating the Blizzard of 1888. Geophysical Research Letters, 40(15), 4092–4097. https://doi.org/10.1002/grl.50750
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