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  2. Eyewall replacement cycle - Wikipedia

    en.wikipedia.org/wiki/Eyewall_replacement_cycle

    Hurricane Beulah in 1967 was the first tropical cyclone to have its eyewall replacement cycle observed from beginning to end. [11] Previous observations of concentric eyewalls were from aircraft-based platforms. Beulah was observed from the Puerto Rico land-based radar for 34 hours during which time a double eyewall formed and dissipated. It ...

  3. Annular tropical cyclone - Wikipedia

    en.wikipedia.org/wiki/Annular_tropical_cyclone

    Tropical cyclones can become annular as a result of eyewall mesovortices mixing the strong winds found in the eyewalls of storms with the weak winds of the eye, which helps to expand the eye. In addition, this process helps to make the equivalent potential temperature (often referred to as theta-e or θ e {\displaystyle \theta _{e}} ) within ...

  4. The Hurricane Rainband and Intensity Change Experiment

    en.wikipedia.org/wiki/The_Hurricane_Rainband_and...

    In tropical cyclones maximum wind speed of the storm, which occurs at the eyewall, is a primary indicator of its overall strength which is important in predicting overall intensity. Just beyond this eyewall is a moat which separates the inner rainbands (eventually the outer eyewall) from the (inner) eyewall.

  5. 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 ...

  6. 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 ...

  7. Central dense overcast - Wikipedia

    en.wikipedia.org/wiki/Central_dense_overcast

    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.

  8. Mesovortex - Wikipedia

    en.wikipedia.org/wiki/Mesovortex

    An eyewall mesovortex is a small-scale rotational feature found in an eyewall of an intense tropical cyclone. Eyewall mesovortices are similar, in principle, to small "suction vortices" often observed in multiple-vortex tornadoes. In these vortices, wind speed can be up to 10% higher than in the rest of the eyewall.

  9. What time is the 'Ring of Fire' eclipse? How to watch ... - AOL

    www.aol.com/time-ring-fire-eclipse-watch...

    An annular eclipse describes the moment the moon passes between the Earth and sun, creating the the illusion of a thin ring of sunlight around the moon. 2:45 p.m. ET: Maximum eclipse beings.