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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...

    Hurricane Ian was a prolific lightning producer as it strengthened into a Category 5 hurricane on its approach to Florida. Storm chasers along the coast of Florida even witnessed cloud-to-ground ...

  3. Eye (cyclone) - Wikipedia

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

    Cross section of a mature tropical cyclone. A typical tropical cyclone has an eye approximately 30–65 km (20–40 mi) across at the geometric center of the storm. The eye may be clear or have spotty low clouds (a clear eye), it may be filled with low-and mid-level clouds (a filled eye), or it may be obscured by the central dense overcast.

  4. Why tornadoes form within hurricanes — and how ... - AOL

    www.aol.com/news/why-tornadoes-form-within...

    The extreme weather associated with Hurricane Milton has included tornadoes that have killed at least five in Florida’s St. Lucie County, a phenomenon known to occur as such storms move inland.

  5. Why Hurricane Milton produced such strong tornadoes - AOL

    www.aol.com/news/why-hurricane-milton-produced...

    Hurricane Milton's tornadoes in Florida were a leading cause of death and damage from the storm. The U.S. has seen an abnormal number of intense tornadoes linked to hurricanes this year.

  6. Eyewall replacement cycle - Wikipedia

    en.wikipedia.org/wiki/Eyewall_replacement_cycle

    Concentric eyewalls seen in Typhoon Haima as it travels west across the Pacific Ocean.. In meteorology, eyewall replacement cycles, also called concentric eyewall cycles, naturally occur in intense tropical cyclones with maximum sustained winds greater than 33 m/s (64 kn; 119 km/h; 74 mph), or hurricane-force, and particularly in major hurricanes of Saffir–Simpson category 3 to 5.

  7. Mesoscale convective complex - Wikipedia

    en.wikipedia.org/wiki/Mesoscale_convective_complex

    These are called "orogenic" complexes. [2] The characteristics of the meteorological environment that MCCs form in are strong warm air advection into the formation environment by a southerly low-level jet stream (wind maximum), strong moisture advection which increases the relative humidity of the formation environment, convergence of air near ...

  8. Rainband - Wikipedia

    en.wikipedia.org/wiki/Rainband

    Some rainbands move closer to the center, forming a secondary, or outer, eyewall within intense hurricanes. [15] Spiral rainbands are such a basic structure to a tropical cyclone that in most tropical cyclone basins , use of the satellite-based Dvorak technique is the primary method used to determine a tropical cyclone's maximum sustained winds ...

  9. Effects of tropical cyclones - Wikipedia

    en.wikipedia.org/wiki/Effects_of_tropical_cyclones

    Shipwrecks are common with the passage of strong tropical cyclones. Such shipwrecks can change the course of history, [7] as well as influence art and literature. A hurricane led to a victory of the Spanish over the French for control of Fort Caroline, and ultimately the Atlantic coast of North America, in 1565. [8]