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  2. From the eye to storm surge: The anatomy of a hurricane - AOL

    www.aol.com/weather/eye-storm-surge-anatomy...

    The center of a tropical system can develop a feature known as an eye. While every storm has a well-defined center, the eye may not be apparent when looking at tropical storms or weaker hurricanes ...

  3. Eye (cyclone) - Wikipedia

    en.wikipedia.org/wiki/Eye_(cyclone)

    The eye is a region of mostly calm weather at the center of a tropical cyclone. The eye of a storm is a roughly circular area, typically 30–65 kilometers (19–40 miles; 16–35 nautical miles) in diameter. It is surrounded by the eyewall, a ring of towering thunderstorms where the most severe weather and highest winds of the cyclone occur.

  4. Eyewall replacement cycle - Wikipedia

    en.wikipedia.org/wiki/Eyewall_replacement_cycle

    The outer eyewall was reported to reach heights near 45,000 feet (14,000 m) while the inner eyewall only extended to 30,000 feet (9,100 m). 12 hours after identifying concentric eyewalls, the inner eyewall had dissipated. [10] Hurricane Beulah in 1967 was the first tropical cyclone to have its eyewall replacement cycle observed from beginning ...

  5. Hurricane Milton - Wikipedia

    en.wikipedia.org/wiki/Hurricane_Milton

    Milton weakened to a Category 4 hurricane after an eyewall replacement cycle, and reintensified into a Category 5 hurricane the following day. [4] [5] Increasing wind shear caused the hurricane to weaken as it turned northeast towards Florida, falling to Category 3 status before making landfall near Siesta Key late on October 9.

  6. WATCH: Storm chaser shows eyewall of Hurricane Milton ... - AOL

    www.aol.com/news/watch-storm-chaser-shows...

    Fox local. FOX 11 Digital Team. October 10, 2024 at 10:03 AM. VENICE, Fla. - Extreme meteorologist and storm chaser Reed Timmer showed what the eyewall of Hurricane Milton looked like as it ...

  7. Mesovortex - Wikipedia

    en.wikipedia.org/wiki/Mesovortex

    A mesovortex is a small-scale rotational feature found in a convective storm, such as a quasi-linear convective system (QLCS, i.e. squall line), a supercell, or the eyewall of a tropical cyclone. [ 1 ][ 2 ] Mesovortices range in diameter from tens of miles to a mile or less [ 3 ] and can be immensely intense.

  8. Central dense overcast - Wikipedia

    en.wikipedia.org/wiki/Central_dense_overcast

    e. The central dense overcast, or CDO, of a tropical cyclone or strong subtropical cyclone is the large central area of thunderstorms surrounding its circulation center, caused by the formation of its eyewall. It can be round, angular, oval, or irregular in shape. This feature shows up in tropical cyclones of tropical storm or hurricane strength.

  9. Tropical cyclone - Wikipedia

    en.wikipedia.org/wiki/Tropical_cyclone

    t. e. A tropical cyclone is a rapidly rotating storm system with a low-pressure center, a closed low-level atmospheric circulation, strong winds, and a spiral arrangement of thunderstorms that produce heavy rain and squalls. Depending on its location and strength, a tropical cyclone is called a hurricane (/ ˈhʌrɪkən, - keɪn /), typhoon ...