This wave initially interacted with the dry Saharan air layer, inhibiting immediate development as it tracked across the eastern Atlantic. Impacts and Legacy Although Hurricane Melissa did not make landfall as a tropical system, its remnants brought significant rainfall and gusty winds to parts of Atlantic Canada.
How Hurricane Melissa Formed: A Detailed Timeline
Understanding the genesis of Hurricane Melissa requires examining the specific environmental conditions that allowed a disorganized cluster of thunderstorms to consolidate into a rotating cyclone with sustained winds reaching hurricane status. This initial formation marked the shift from a mere atmospheric disturbance to a organized tropical system with a defined center of rotation.
Environmental Conditions and Intensification The intensification of Tropical Depression Fifteen into Tropical Storm Melissa was driven by exceptionally favorable conditions in its path. Sea surface temperatures in the storm's trajectory were running 1 to 2 degrees Celsius above average, providing ample heat and moisture to fuel the storm's convection.
How Hurricane Melissa Formed: Tracking the Timeline from Tropical Wave to Atlantic Canada
Tropical Origins and Wave Development The story of Hurricane Melissa begins with a tropical wave, a low-pressure trough of air moving westward off the coast of West Africa. However, as the wave progressed westward, it entered a region of the atmosphere characterized by decreasing wind shear and warmer sea surface temperatures.
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