
What are the disadvantages of Cyclones?
Answer
397.8k+ views
Hint: In the Northern Hemisphere, a cyclone is a system of winds rotating counterclockwise around a low-pressure center. Clouds and precipitation form as the swirling air rises and cools. Tropical cyclones and middle latitude (mid-latitude) cyclones are the two types of cyclones.
Complete answer:
A cyclone is a large-scale air mass that rotates counterclockwise in the Northern Hemisphere and clockwise in the Southern Hemisphere as seen from above, rotating around a strong center of low atmospheric pressure (opposite to an anticyclone).
Cyclones are defined by inward-spiraling winds that revolve around a low-pressure zone. Polar vortices and extratropical cyclones of the largest scale are the largest low-pressure systems (the synoptic scale). Tropical and subtropical cyclones, as well as warm-core cyclones, are included in the synoptic scale. Smaller mesoscale features include mesocyclones, tornadoes, and dust devils.
During the summer months in the Northern Hemisphere, upper-level cyclones can form without the presence of a surface low, pinching off from the base of the tropical upper tropospheric trough. Cyclones have also been observed on planets beyond our solar system, including Mars, Jupiter, and Neptune.
Cyclones have the following disadvantages:
> It causes seas to flood.
> Cyclones are known for wreaking havoc on people and property on a large scale.
> It could be the source of disease transmission.
> Cyclones bring a lot of rain, which has an impact on agriculture.
Note:
The development or strengthening of cyclonic circulation in the atmosphere is known as cyclogenesis. Cyclogenesis is a catch-all term for a variety of processes that all result in the formation of a cyclone. It can occur on a variety of scales, ranging from the micro to the synoptic.
Complete answer:
A cyclone is a large-scale air mass that rotates counterclockwise in the Northern Hemisphere and clockwise in the Southern Hemisphere as seen from above, rotating around a strong center of low atmospheric pressure (opposite to an anticyclone).
Cyclones are defined by inward-spiraling winds that revolve around a low-pressure zone. Polar vortices and extratropical cyclones of the largest scale are the largest low-pressure systems (the synoptic scale). Tropical and subtropical cyclones, as well as warm-core cyclones, are included in the synoptic scale. Smaller mesoscale features include mesocyclones, tornadoes, and dust devils.
During the summer months in the Northern Hemisphere, upper-level cyclones can form without the presence of a surface low, pinching off from the base of the tropical upper tropospheric trough. Cyclones have also been observed on planets beyond our solar system, including Mars, Jupiter, and Neptune.
Cyclones have the following disadvantages:
> It causes seas to flood.
> Cyclones are known for wreaking havoc on people and property on a large scale.
> It could be the source of disease transmission.
> Cyclones bring a lot of rain, which has an impact on agriculture.
Note:
The development or strengthening of cyclonic circulation in the atmosphere is known as cyclogenesis. Cyclogenesis is a catch-all term for a variety of processes that all result in the formation of a cyclone. It can occur on a variety of scales, ranging from the micro to the synoptic.
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