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Mahesh

16/10/24 11:34 AM IST

Swell waves

In News
  • The Indian National Centre for Ocean Information Services (INCOIS) in Hyderabad, an autonomous body under the Union Ministry of Earth Sciences, has issued extensive advisories for swell waves for Andaman and Nicobar and Lakshadweep islands.
Swell Waves
  • Swell waves are long-wavelength ocean waves that travel away from their places of origin.
  • They are usually created by windstorms or other weather systems. Sea waves otherwise are usually generated due to local winds.
  • Windstorms and other powerful air current systems transfer energy from the air to water, making swell waves more powerful than locally generated waves.
  • Because of their high energy, swell waves are able to travel large distances and strike shores with considerably high power.
  • According to INCOIS, swell waves organise themselves into groups of similar heights and periods, and then travel long distances without much change. 
  • Wave period is the time one wavelength takes to pass a specific point.
  • Longer wavelengths, therefore, result in longer wave periods, and these characteristics are associated with faster and more powerful waves.
  • A wave is essentially a transfer of energy from one point to another.
  • Shorter waves dissipate more energy due to frequent movement, which is why they also lose energy quickly.
  • Longer wavelengths are more powerful, and this is also why swells continue to persist days after they are formed.
  • Direction is also important characteristics associated with swells. Meteorologists forecast swell directions in degrees that indicate the direction where the swell is coming from.
Kallakkadal waves
  • Kallakkadal waves inundate large areas of land when the sudden waves surge.
  • These waves are also sometimes confused with tsunami waves given their stealthy nature, but both are different.
  • Kallakkadal waves are caused due to weather phenomenon, while tsunamis are mostly caused due to earthquakes or tectonic activity.
  • A 2016 study by INCOIS found that meteorlogical conditions in the Southern Indian Ocean, including strong and long duration surface winds, generate favourable conditions for long-period swells.
  • High-waves in the Southern Indian Ocean can also propagate to the north as swells, causing Kallakkadal events along the North Indian Ocean coastal regions. 
Source- The Hindu

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