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High-Energy Swell Waves
Why in News:
INCOIS issued alerts for high-energy waves along coastal states.
More in news:
Leading to the suspension of beach activities, Kerala is on red alert due to the ‘Kallakadal’ phenomenon, which poses flood risks.
Swell Waves:
- Swells are generated by wind blowing over the ocean’s surface.
- “Storms produce powerful waves due to strong, prolonged winds over vast distances”.
- The strength, duration, and area of wind determine the size and power of waves.
- Swell energy diminish as waves move away from the storm source.
- They Can combine with others, gaining energy or dissipating.
- Two types of swells:
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- Groundswell from distant winds, resulting in longer, organized waves;
- Windswell from nearby winds, creating shorter, less organized waves.
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- Swell direction is described in degrees from North to South.
- The angle of the swell and coastline features determine surf conditions.
- Island blockage can reduce swell energy, affecting surf quality.
- Swell characteristics, local conditions, weather, and tides interact to create surf conditions.
About the High-Energy Swell Waves:
- It originates from the southern Atlantic Ocean and majorly hit the Indian coastal regions, starting from the southern tip of India.
- These swells, combined with high tide conditions, could cause coastal flooding, particularly in low-lying areas.
The Phenomenon ‘Kallakadal’ (Rogue Sea):
- ‘Kallakadal’, a local term, refers to the phenomenon of high-energy swell waves.
- Kerala, in particular, is on red alert for these waves.
- Swell waves could reach heights of 0.5 to 1.7 meters, posing a risk to low-lying areas.