Abstract
Cyclone tracks over the Great Lakes of North America shift, both East–West as well as North–South. The reasons for the shifts are various small-scale as well as large-scale processes associated with the general circulation of the atmosphere. The East–West shift has an approximate periodicity of 10 years, while the North–South shift occurs roughly with a periodicity of 20 years. The East–West shift is more important than the North–South shift. The amount of shift could be as much as a few hundred kilometers. The implication of these shifts for storm surges in the Great Lakes is considered.
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Mahdi, TF., Jain, G., Patel, S. et al. A review of cyclone track shifts over the Great Lakes of North America: implications for storm surges. Nat Hazards 98, 119–135 (2019). https://doi.org/10.1007/s11069-018-3429-2
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DOI: https://doi.org/10.1007/s11069-018-3429-2