Consider the following conditions favourable for the formation and intensification of Tropical Storms :
- Presence of the Coriolis force
- Upper divergence above the sea level system
- High variations in the vertical wind speed
Which of the conditions given above is/are correct ?
- AOption (a)
1 only
- BOption (b)
2 only
- COption (c)
1 and 2
- DOption (d)
2 and 3
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Correct answer
1 and 2
Why this answer is correct
The correct answer is 1 and 2.
Key Points
- Presence of the Coriolis force:
- The Coriolis force is essential for the formation of a tropical storm. It causes the deflection of wind patterns, making the storm rotate. This is why tropical storms do not form near the equator (where the Coriolis force is minimal or absent). Hence, this statement is correct.
- Upper divergence above the sea level system:
- Upper-level divergence promotes the intensification of a tropical storm. It allows air to rise from the surface, which is a critical process in the development of a low-pressure system. Hence, this statement is correct.
- High variations in vertical wind speed:
- High variations in vertical wind speed (also called wind shear) are not favorable for the development of tropical storms. Wind shear disrupts the vertical structure of the storm and prevents it from growing. Therefore, minimal wind shear is crucial for the storm's formation and intensification. Hence, this statement is incorrect.
- Based on the above, only statements 1 and 2 are correct.
Additional Information
- Tropical Storms:
- Tropical storms are intense low-pressure systems that develop over warm ocean waters in tropical and subtropical regions.
- These storms are characterized by strong winds (above 63 km/h), heavy rainfall, and thunderstorms. When wind speeds exceed 119 km/h, the storm is classified as a cyclone, hurricane, or typhoon, depending on the region.
- Role of Warm Ocean Waters:
- Sea surface temperatures above 26.5°C provide the necessary heat and moisture for the formation of tropical storms.
- The warm water evaporates, fueling the storm with latent heat energy.
- Regions of Formation:
- Tropical storms typically form between 5° and 30° latitude in both hemispheres, where the Coriolis force is significant enough to initiate rotation.
- Examples include the Atlantic Ocean (hurricanes), Pacific Ocean (typhoons), and the Indian Ocean (cyclones).
- Stages of Development:
- Formation: Warm ocean waters and low-pressure systems initiate storm development.
- Growth: Rising warm air creates a central low-pressure area, with the Coriolis force causing rotation.
- Intensification: Low wind shear and favorable atmospheric conditions allow the storm to grow stronger.
- Dissipation: The storm weakens when it moves over cooler waters or land, cutting off its energy source.
- Impact of Wind Shear:
- Wind shear refers to changes in wind speed and direction with altitude.
- High wind shear can disrupt the vertical alignment of a storm, weakening or preventing its development.
- Minimal wind shear is ideal for the formation and growth of tropical storms.
Important Points
- Global Warming and Tropical Storms:
- Rising global temperatures may increase the frequency and intensity of tropical storms due to warmer ocean waters.
- Studies suggest that climate change could lead to more intense storms, with higher wind speeds and increased precipitation.
- Notable Tropical Storms:
- Hurricane Katrina (2005) – One of the costliest hurricanes in U.S. history.
- Typhoon Haiyan (2013) – A devastating storm that affected the Philippines.
- Cyclone Fani (2019) – A powerful tropical cyclone that hit India and Bangladesh.