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  2. Cyclogenesis - Wikipedia

    en.wikipedia.org/wiki/Cyclogenesis

    Mesocyclones form as warm core cyclones over land, and can lead to tornado formation. Waterspouts can also form from mesocyclones, but more often develop from environments of high instability and low vertical wind shear. The process in which an extratropical cyclone undergoes a rapid drop in atmospheric pressure (24 millibars or more) in a 24 ...

  3. Tropical cyclogenesis - Wikipedia

    en.wikipedia.org/wiki/Tropical_cyclogenesis

    Tropical cyclones typically began to weaken immediately following and sometimes even prior to landfall as they lose the sea fueled heat engine and friction slows the winds. However, under some circumstances, tropical or subtropical cyclones may maintain or even increase their intensity for several hours in what is known as the brown ocean ...

  4. Portal:Tropical cyclones - Wikipedia

    en.wikipedia.org/wiki/Portal:Tropical_cyclones

    A "Typhoon" is a tropical cyclone located in the North-west Pacific Ocean which has the most cyclonic activity and storms occur year-round. 2. A "Hurricane" is also a tropical cyclone located at the North Atlantic Ocean or North-east Pacific Ocean which have an average storm activity and storms typically form between May 15 and November 30. 3.

  5. Cyclone - Wikipedia

    en.wikipedia.org/wiki/Cyclone

    Occluded fronts form late in the cyclone life cycle near the center of the cyclone and often wrap around the storm center. Tropical cyclogenesis describes the process of development of tropical cyclones. Tropical cyclones form due to latent heat driven by significant thunderstorm activity, and are warm core.

  6. Tropical cyclone - Wikipedia

    en.wikipedia.org/wiki/Tropical_cyclone

    A subtropical cyclone is a weather system that has some characteristics of a tropical cyclone and some characteristics of an extratropical cyclone. They can form in a wide band of latitudes, from the equator to 50°. Although subtropical storms rarely have hurricane-force winds, they may become tropical in nature as their cores warm. [121]

  7. Mesoscale convective system - Wikipedia

    en.wikipedia.org/wiki/Mesoscale_convective_system

    They tend to form near weather fronts and move into areas of 1000-500 mb thickness diffluence, which are areas where the low to mid level temperature gradient broadens, which generally steers the thunderstorm clusters into the warm sector of extratropical cyclones, or equatorward of warm fronts. They can also form along any convergent zones ...

  8. Outline of tropical cyclones - Wikipedia

    en.wikipedia.org/wiki/Outline_of_tropical_cyclones

    Cumulative graph of tropical cyclones in the eastern Pacific. Tropical cyclone – a rapidly rotating low-pressure system consisting of a spiral band of thunderstorms, strong winds, and atmospheric circulation that can produce heavy rain and squalls. Depending on the location, they are given different names such as hurricanes, cyclones, or ...

  9. Tropical cyclones and climate change - Wikipedia

    en.wikipedia.org/wiki/Tropical_cyclones_and...

    The majority of these systems form each year in one of seven tropical cyclone basins, which are monitored by a variety of meteorological services and warning centres. The factors that determine tropical cyclone activity are relatively well understood: warmer sea levels are favourable to tropical cyclones, as well as an unstable and moist mid ...

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