See Cyclone Live location

See Cyclone Live location

In meteorology, a cyclone is a large scale air mass that rotates around a strong centre of low atmospheric pressure. Cyclones are characterized by inward spiralling winds that rotate about a zone of low pressure. The largest low-pressure systems are polar vortices and extratropical cyclones of the largest scale (the synoptic scale). Warm-core cyclones such as tropical cyclones and subtropical cyclones also lie within the synoptic scale. Mesocyclones, tornadoes, and dust devils lie within smaller mesoscale. Upper-level cyclones can exist without the presence of a surface low and can pinch off from the base of the tropical upper tropospheric trough during the summer months in the Northern Hemisphere. Cyclones have also been seen on extraterrestrial planets, such as Mars, Jupiter, and Neptune. 


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There are a number of structural characteristics common to all cyclones. A cyclone is a low-pressure area. A cyclone's centre (often known in a mature tropical cyclone as the eye), is the area of lowest atmospheric pressure in the region. Near the centre, the pressure gradient force (from the pressure in the centre of the cyclone compared to the pressure outside the cyclone) and the force from the Coriolis effect must be in an approximate balance, or the cyclone would collapse on itself as a result of the difference in pressure. 

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A surface low can form in a variety of ways. Topography can create a surface low. Mesoscale convective systems can spawn surface lows that are initially warm core. The disturbance can grow into a wave-like formation along the front and the low is positioned at the crest. Around the low, the flow becomes cyclonic. This rotational flow moves polar air towards the equator on the west side of the low, while warm air move towards the pole on the east side. 

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Windy is a Czech company providing interactive weather forecasting services worldwide. The portal was founded by Ivo Lukačovič in November 2014. Currently, weather forecasts are based on data from the GFS models.
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