primarily associated with a tropical wave that left the West coast of Africa on October 11th, 2012 (Blake, Todd, 2012). The large tropical wave encountered a large upper-level trough over the eastern Atlantic a couple days after leaving Africa which resulted in an extensive area of showers and thunderstorms, but was not strong enough for the development of the hurricane itself (Eric S. Blake, Todd B, 2012). The wave then began to produce little convection near the wave axis for another couple days and…
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