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- W2593646087 abstract "Predicting the development, structure, movement, intensity, and total snowfall of lake-effect (LE) snowstorms continues to be a challenge for weather forecast offices in the Great Lakes region (e.g., Rothrock 1969, Niziol 1987, Burrows 1991, Niziol et al. 1995, Sousounis et al. 1999). These storms can often produce significant snow accumulations within very short time periods which may negatively impact transportation systems, limit business operations, cause significant property damage, and result in injuries and deaths due to accidents and exertion (Schmidlin 1993, Schmidlin and Kosarik 1999). The difficulty in predicting the development and evolution of LE snowstorms rests with the numerous parameters that influence the LE system (e.g., Hjelmfelt 1990, Laird et al. 2003a) and the complex atmospheric circulations that exist and interact across various spatial and temporal scales. The LE storms that frequently result in the greatest impacts are mesoscale systems typically associated with an individual lake. These systems are often characterized by a distinct morphology that may include widespread coverage, typically comprised of windparallel horizontal roll convection (e.g., Kristovich 1993, Kristovich and Laird 1998), shoreline bands (e.g., Passarelli and Braham 1981, Ballentine et al. 1998), mesoscale vortices (e.g., Forbes and Merritt 1984, Laird 1999) or an amalgamation of several morphologies. For this study, historically separated classifications of shore-parallel and mid-lake bands are consolidated into a single morphological regime called shoreline bands. Across the range of shoreline band events, overlake mesoscale low pressure and lower-tropospheric convergence occurs as a result of a linkage and balance between dynamical and surface diabatic forcing. Even though band intensity and position relative to the shoreline may differ depending on the primary forcing, the resulting LE morphology is often a single, coherent shoreline band capable of significant snowfall. An additional reason for consolidating shore-parallel and mid-lake bands into the shoreline band category was the use of LE cases identified by past studies. Not all previous studies have used the traditional LE classifications or have provided enough information to effectively discriminate between shore-parallel and mid-" @default.
- W2593646087 created "2017-03-16" @default.
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- W2593646087 date "2004-01-01" @default.
- W2593646087 modified "2023-09-28" @default.
- W2593646087 title "Utilizing idealized mesoscale model simulations to aid the prediction of lake-effect snowstorms" @default.
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