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- Tropical cyclones form in specific conditions within the tropics12345:
- Warm ocean waters (at least 80°F / 27°C) throughout a depth of about 150 ft.
- An atmosphere that cools fast enough with height to be potentially unstable to moist convection.
- Relatively moist air near the mid-level of the troposphere (16,000 ft. / 4,900 m).
- A minimum distance of at least 300 miles (480 km) from the equator.
- They usually form between approximately 5° and 30° latitude.
Learn more:✕This summary was generated using AI based on multiple online sources. To view the original source information, use the "Learn more" links.Tropical oceans spawn approximately 80 tropical storms annually, and about two-thirds are severe (category 1 or higher on the Saffir-Simpson scale of intensity). Almost 90 percent of these storms form within 20° north or south of the Equator.www.britannica.com/science/tropical-cyclone/Locat…Tropical cyclones cannot form outside of the tropics because the water temperatures are too cold A warm, moist tropical atmosphere Encourages thunderstorm development, the foundation of the latent heat release process that drives tropical cyclones More than 500 kilometres (about 5° latitude) away from the equatorwww.canada.ca/en/environment-climate-change/se…For a tropical storm to form, there needs to be a warm ocean (27 °C or above) and light winds. As tropical storms require warm oceans, they are normally found in tropical regions between 5° and 30° north and south of the equator where the water is warmest. They usually form in the late summer when sea temperatures are at their highest.www.bbc.co.uk/bitesize/topics/zn476sg/articles/zk8…Cyclones form between approximately 5° and 30° latitude. Because of easterly winds they initially move westward. They occur most commonly in early autumn as this is when sea temperatures are at their highest, temperatures having built up over the summer.www.bbc.co.uk/bitesize/guides/z9whg82/revision/2They are:
- Warm ocean waters (at least 80 °F / 27 °C) throughout a depth of about 150 ft. (46 m ).
- An atmosphere which cools fast enough with height such that it is potentially unstable to moist convection. ...
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