Tew-Fik Mahdi, Gaurav Jain, Shay Patel et Aman Kaur Sidhu
Article de revue (2019)
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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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| Département: | Département des génies civil, géologique et des mines |
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| URL de PolyPublie: | https://publications.polymtl.ca/5317/ |
| Titre de la revue: | Natural Hazards (vol. 98, no 1) |
| Maison d'édition: | Springer |
| DOI: | 10.1007/s11069-018-3429-2 |
| URL officielle: | https://doi.org/10.1007/s11069-018-3429-2 |
| Date du dépôt: | 13 juil. 2020 18:12 |
| Dernière modification: | 08 avr. 2025 13:05 |
| Citer en APA 7: | Mahdi, T.-F., Jain, G., Patel, S., & Sidhu, A. K. (2019). A review of cyclone track shifts over the Great Lakes of North America: implications for storm surges. Natural Hazards, 98(1), 119-135. https://doi.org/10.1007/s11069-018-3429-2 |
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