When.com Web Search

Search results

  1. Results From The WOW.Com Content Network
  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. Project Stormfury - Wikipedia

    en.wikipedia.org/wiki/Project_Stormfury

    The new theory took cumulus towers outside the eyewall into account. According to the revised theory, by seeding the towers, latent heat would be released. This would trigger the start of new convection, which would then cause a new eyewall. Since the new eyewall was outside the original one, the first eyewall would be choked of energy and fall ...

  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. Hurricane Isabel - Wikipedia

    en.wikipedia.org/wiki/Hurricane_Isabel

    After completing the replacement cycle, the hurricane's large 40 miles (64 km) wide eye became better defined, [14] and late on September 13, Isabel re-attained Category 5 status. [1] During this time, Isabel attained annular characteristics, becoming highly symmetrical in shape and sporting a wide eye. [1]

  9. Portal : Tropical cyclones/Featured article/Eye (cyclone)

    en.wikipedia.org/wiki/Portal:Tropical_cyclones/...

    In strong tropical cyclones, the eye is characterized by light winds and clear skies, surrounded on all sides by a towering, symmetric eyewall. In weaker tropical cyclones, the eye is less well-defined, and can be covered by the central dense overcast , which is an area of high, thick clouds which show up brightly on satellite imagery .