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Understanding Tropical Cyclones

Tropical cyclones, also called hurricanes or typhoons, are powerful storms that form over warm ocean waters and can cause widespread destruction. They require specific conditions to develop, such as warm sea temperatures and low wind shear. These storms play a crucial role in redistributing heat on Earth and can have significant environmental and societal impacts, especially in coastal regions. Understanding their formation, tracking, and predicting their paths are vital for preparedness and minimizing damage.

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1

Intense circular storm systems with a low-pressure center and high winds are known as ______ in the Atlantic and northeastern Pacific.

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hurricanes

2

The term 'tropical cyclones' is commonly used for these storms in the ______ Ocean and ______ Pacific.

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Indian South

3

Globally, about ______ to ______ tropical cyclones form each year, with over half becoming strong enough to be classified as hurricane-force.

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80 90

4

Tropical cyclones play a crucial role by moving heat from the ______ regions to higher latitudes, affecting the Earth's ______ system.

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equatorial climate

5

Energy source for tropical cyclones

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Tropical cyclones draw energy from moisture evaporating from warm ocean waters.

6

Size range of tropical cyclones

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Diameters of tropical cyclones vary from 100 to 2000 kilometers.

7

Impact of tropical cyclones on coastal areas

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Coastal regions can experience destructive winds, torrential rains, high waves, storm surges, and sometimes tornadoes.

8

Heavy rainfall from tropical cyclones may cause ______ and ______ flooding in inland regions.

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riverine flash

9

Regions like the ______ ______ in the U.S., parts of ______ ______, ______ and the ______ subcontinent are highly vulnerable to cyclones.

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Gulf Coast Southeast Asia Australia Indian

10

The ______ ______ is believed to potentially increase the severity and modify the patterns of tropical cyclones.

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changing climate

11

Minimum sea surface temperature for tropical cyclone genesis

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27°C (81°F) is the threshold SST for tropical cyclone formation.

12

Factors limiting tropical cyclone intensity

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Water temperature below and atmospheric conditions above, including upper-level winds, are key constraints.

13

Annual average statistics for tropical cyclones

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86 reach tropical storm strength, 47 become hurricanes or typhoons, and about 20 escalate to major cyclones (Category 3+).

14

The ______ and ______ are climatic phenomena that can affect tropical cyclone formation.

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El Niño–Southern Oscillation Madden–Julian oscillation

15

______ and ______ waves can play a role in the development and intensification of tropical cyclones.

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Rossby Kelvin

16

The ______ is responsible for designating centers that track and forecast tropical cyclones.

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World Meteorological Organization

17

Advisories on tropical cyclones include information on their current and expected ______, ______, and ______.

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path movement intensity

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Understanding Tropical Cyclones

Tropical cyclones are intense circular storm systems that feature a low-pressure center, high winds, and a spiral arrangement of thunderstorms yielding heavy rainfall. Depending on their location and intensity, these storms are referred to as hurricanes, typhoons, or simply cyclones. In the Atlantic and northeastern Pacific, they are called hurricanes, while in the northwestern Pacific, they are known as typhoons. Elsewhere, including the Indian Ocean and South Pacific, the term "tropical cyclones" is used. On average, 80 to 90 tropical cyclones develop annually around the world, with more than half reaching hurricane-force winds of at least 65 knots. These storms are essential in the Earth's climate system, redistributing heat from the equatorial regions to higher latitudes.
Satellite view of a tropical cyclone with a spiral structure and a clear eye in the center, surrounded by dense cloud bands in shades of white and gray.

Formation and Characteristics of Tropical Cyclones

Tropical cyclones originate over warm ocean waters, drawing energy from the moisture that evaporates from the sea surface. This process is different from the formation of mid-latitude cyclones, which are driven by contrasts in atmospheric temperature. The size of tropical cyclones can vary widely, with diameters ranging from 100 to 2000 kilometers. Their rotation is influenced by the Earth's rotation through the Coriolis effect, which is why they do not form near the equator (typically within 5° latitude). Tropical cyclones are most powerful over warm waters and tend to dissipate quickly over land. Coastal areas are thus highly susceptible to the damaging effects of these storms, which can include destructive winds, torrential rains, high waves, storm surges, and occasionally tornadoes.

The Impact of Tropical Cyclones on the Environment and Human Populations

The environmental and societal impacts of tropical cyclones can be profound. They often cause severe coastal erosion, property damage, and can compromise flood defenses. Inland areas are not immune, as heavy rainfall can lead to riverine and flash flooding. Human communities, particularly in regions such as the Gulf Coast of the United States, parts of Southeast Asia, Australia, and the Indian subcontinent, can suffer catastrophic consequences. The changing climate may exacerbate the effects of tropical cyclones by increasing their intensity, altering their frequency, and shifting the patterns of their tracks.

The Science Behind Tropical Cyclone Development

The genesis of tropical cyclones is complex, requiring several environmental conditions to coincide. These include sea surface temperatures of at least 27°C (81°F), low vertical wind shear, atmospheric instability, ample moisture in the lower to mid-troposphere, a sufficient Coriolis effect to initiate rotation, and a pre-existing weather disturbance. The intensity of a tropical cyclone is constrained by the temperature of the water beneath it and the atmospheric conditions above it, such as the presence of upper-level winds that promote outflow. Statistically, an average of 86 tropical cyclones reach tropical storm strength each year, with 47 escalating to hurricane or typhoon strength, and about 20 becoming major tropical cyclones (Category 3 or above on the Saffir–Simpson Hurricane Wind Scale).

Monitoring and Predicting Tropical Cyclones

The tracking and forecasting of tropical cyclones are critical for mitigating their potential impacts. Meteorological organizations around the globe, including Regional Specialized Meteorological Centres and Tropical Cyclone Warning Centres designated by the World Meteorological Organization, monitor these storms and issue timely advisories. These advisories provide updates on the current and projected path, movement, and intensity of tropical cyclones. Climatic phenomena such as the El Niño–Southern Oscillation and the Madden–Julian oscillation can influence the timing and frequency of tropical cyclone formation. Additionally, atmospheric waves like Rossby and Kelvin waves can contribute to the development and strengthening of these powerful storms.