SWELL WAVES - GEOGRAPHY

News: Swell waves likely to hit several coastal areas

 

What's in the news?

       The Indian National Centre for Ocean Information Services (INCOIS) forecasted that high sea waves/ swell waves might hit both the west and east coasts of India and Lakshadweep and A&N Islands between May 4 and 5.

 

Swell Waves:

       These waves are formed by an ocean swell, hence the name swell surge.

       Ocean swells occur not due to the local winds, but rather due to distant storms like hurricanes or even long periods of fierce gale winds.

       During such storms, huge energy transfer takes place from the air into the water, leading to the formation of very high waves.

       These swell waves can travel thousands of kilometres from the storm centre until they strike shore.

 

Swell Surge Forecast System:

       To forecast swell waves, INCOIS launched the Swell Surge Forecast System in 2020 which can give warning seven days in advance.

 

Vulnerable Regions for Swell Waves in India:

       Usually, states like Kerala witness swell waves as a result of strong winds in the southern part of the Indian Ocean.

       In March 2024, swell waves led to flooding in several areas of Kerala - the worst affected were Alappuzha, Kollam, and Thiruvananthapuram districts. Such flooding events are called Kallakkadal in Kerala.

 

Difference Between Swell Waves and Tsunamis:

       Unlike swell waves, a tsunami is a series of enormous waves created by an underwater disturbance usually associated with earthquakes occurring below or near the ocean.

       Tsunamis are around 10 times faster than swell waves. Although both swell waves and tsunamis slow down near the coast, the latter hit land at 30–50 km/h.

 

Go back to basics:

Kallakkadal:

       ‘Kallakkadal’ is a colloquial term used by Kerala fishermen to refer to flash flooding events.

       In Malayalam, Kallan means thief or mischievous one and Kadal means sea.

       Fishermen use the term ‘Kalla Kadal’ to refer to the unusual occurrence of high swell waves during good weather.

       According to weather experts, the phenomenon is triggered by storms as far away as the Antarctic region.

 

Features:

       Kallakkadal are caused by meteorological conditions in the Southern Ocean, south of 30°S.

       After travelling thousands of kilometres across the ocean basin, the swell intensifies when it encounters a coastal current, a phenomenon known as remote forcing.

       'Kalla Kadal' usually occurs along the southern coast of India, mainly during the pre-monsoon period, in April and May during clear weather conditions.

       In 2012, UNESCO formally accepted the term for scientific use.