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A review of cyclone track shifts over the Great Lakes of North America: implications for storm surges

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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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Fig. 1

(Reproduced with permission from Wikimedia Commons contributors 2014)

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(Reproduced with permission from NAV Canada 2017)

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(Reproduced with permission from NAV Canada 2017)

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(Reproduced with permission from Birchfield and Murty 1974)

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(Reproduced with permission from Birchfield and Murty 1974)

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(Reproduced with permission from Murty and Polavarapu 1975)

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(Reproduced with permission from Murty and Polavarapu 1975)

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(Reproduced with permission from Murty and Polavarapu 1975)

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(Reproduced with permission from Freeman and Murty 1972)

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(Reproduced with permission from Freeman and Murty 1972)

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(Reproduced with permission from Freeman and Murty 1972)

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(Reproduced with permission from Murty and Freeman 1973)

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Correspondence to Tew-Fik Mahdi.

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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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