What is Kallakkadal?
(கள்ளக் கடல்)
Why in News?
Recently, hundreds of houses have been flooded in several coastal areas of Kerala due to high sea waves named Kallakkadal.
Lakshadweep and Tamil Nadu coast are other areas often affected by Kallakkadal.
Kallakkadal refers to coastal flooding caused by swell waves (different from ordinary waves) during the pre-monsoon season (April-May) and sometimes during post monsoon along the southwest coast of India.
The term Kallakkadal, used by local fishermen, is a combination of two Malayalam words, including Kallan and Kadal.
“Kallan means thief and Kadal means sea, meaning “ocean that arrives as a thief".
It is caused by waves formed by ocean swells, which originate from distant storms such as hurricanes or prolonged periods of intense gale winds (usually in the southern part of the Indian Ocean).
These storms transfer significant energy from the air into the water, resulting in the formation of extremely high waves.
These waves can travel vast distances from the storm centre until they reach the shoreline.
Kallakkadal occurs without precursors or any kind of local wind activity and as a result, it has been very difficult for the coastal population to get an advance warning.
However, early warning systems like the Swell Surge Forecast System —launched by the Indian National Centre for Ocean Information Services (INCOIS) gives forewarning seven days in advance.
Why is Kallakkadal Different from Tsunami?
Kallakkadal came under the spotlight after the 2004 tsunami. It is often mistaken for a tsunami.
A tsunami is a series of enormous waves created by an underwater disturbance, usually associated with earthquakes occurring below or near the ocean.
Kallakkadal waves have a wavelength of only 30 or 40 meters, tsunamis have a very long wavelength often hundreds of kilometers long.
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