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  2. Effects of tropical cyclones - Wikipedia

    en.wikipedia.org/wiki/Effects_of_tropical_cyclones

    The exports and imports are halted in sea ports due to the cyclone. Some people lose their jobs as well. A mature tropical cyclone can release heat at a rate upwards of 6×10 14 watts. [1] Tropical cyclones on the open sea cause large waves, heavy rain, and high winds, disrupting international shipping and, at times, causing shipwrecks. [2]

  3. Fujiwhara effect - Wikipedia

    en.wikipedia.org/wiki/Fujiwhara_effect

    Typhoon Parma (left) and Melor (right) interacting with each other in the Philippine Sea on October 6, 2009.. The Fujiwhara effect, sometimes referred to as the Fujiwara effect, Fujiw(h)ara interaction or binary interaction, is a phenomenon that occurs when two nearby cyclonic vortices move around each other and close the distance between the circulations of their corresponding low-pressure areas.

  4. Tropical cyclone - Wikipedia

    en.wikipedia.org/wiki/Tropical_cyclone

    Extratropical cyclones can also be dangerous when their low-pressure centers cause powerful winds and high seas. [120] 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°.

  5. Cyclone - Wikipedia

    en.wikipedia.org/wiki/Cyclone

    Upper cyclones and the upper troughs that trail tropical cyclones can cause additional outflow channels and aid in their intensification. Developing tropical disturbances can help create or deepen upper troughs or upper lows in their wake due to the outflow jet emanating from the developing tropical disturbance/cyclone.

  6. Explainer-What are bomb cyclones and how do they form? - AOL

    www.aol.com/news/explainer-bomb-cyclones-form...

    A bomb cyclone's winds can reach hurricane force - 74 miles (119 km) per hour - and stronger. These storms tend to form during winter and can spawn copious amounts of precipitation.

  7. Eyewall replacement cycle - Wikipedia

    en.wikipedia.org/wiki/Eyewall_replacement_cycle

    Tropical cyclones are fuelled by the high ocean temperature. Sea surface temperatures immediately underneath a tropical cyclone can be several degrees cooler than those at the periphery of a storm; cyclones depend on receiving energy from the ocean transported by the inward spiralling winds. When an outer eyewall is formed, the moisture and ...

  8. 2nd bomb cyclone, atmospheric river in three days to ... - AOL

    www.aol.com/weather/2nd-bomb-cyclone-atmospheric...

    A bomb cyclone is a storm that strengthens so fast that the central atmospheric pressure plunges 0.71 of an inch (24 millibars) or more in 24 hours or less. The central pressure in Tuesday's bomb ...

  9. Radius of outermost closed isobar - Wikipedia

    en.wikipedia.org/wiki/Radius_of_outermost_closed...

    As tropical cyclones weaken, their ROCI values diminish. In general, the size of a tropical cyclone shows little relation to its intensity. Use of this measure has objectively determined that tropical cyclones in the northwest Pacific Ocean are the largest on earth on average, with North Atlantic tropical cyclones roughly half their size. [3]