Kallakkadal
An editor has nominated this article for deletion. You are welcome to participate in the deletion discussion, which will decide whether or not to retain it. |
Kallakadal or swell surge waves are coastal flash flood events that take place without any noticeable advance change in local winds or any other apparent signature in the coastal environment. It is derived from a Malayalam word meaning 'thief-like waves'. Kallakkadal events are considered as a growing climatic change risk along the Indian coasts and these are caused by high swell waves, without any sign in the local winds, sometimes cause severe flooding. Other local terms for such events include Rissaga in the Balearic islands.[1]
Description
[edit]A recent research focused on the causes of Kallakkadal events[2] has established the link between North Indian Ocean high swell events and the meteorological conditions in the Southern Ocean using a combination of ocean wave observations and numerical model simulations. The study confirms that Kallakkadal events are caused by swells propagating from the Southern Indian Ocean of 30°S, from the region between Africa and Australia. Swell waves are generated by distant weather systems, where wind blows for a duration of time over a large fetch.[3]
The long period swell waves (>18 s) seen during Kallakkadal/Swell surge events are generated in the southern Indian Ocean by severe low pressure system existed 3–5 days prior to the Kallakkadal events. The quasi-stationary nature of the southern ocean low pressure systems provides strong (~25 ms-1) and long duration (~3 days) surface winds over a large fetch; essential conditions for the generation of long period swells. The intense winds associated with these severe low pressure systems in the Southern Indian Ocean trigger the generation of high waves which propagate to Indian Coastal regions as swells.[3] Furthermore, these swells affect coastal areas which are dependent on the local topography, angle of incidence and tidal conditions, cause high wave activity and Kallakkadal along the Indian coastal regions. The study shows that Kallakkadal events along NIO coasts can be effectively monitored and forecasted at least 2 days in advance if the meteorological conditions of the Southern Ocean are properly monitored. INCOIS has been now successfully giving advanced warning to the coastal community about the Kallakkadal events.[citation needed]
Characteristics of Kallakadal
[edit]Characteristics of “Kallakkadal” include an annual occurrence. It involves intense wave activity that continues for several days and is unrelated to local weather and is known from the southern Kerala region.
- This phenomenon occurs mostly during pre-monsoon season and sometimes during post monsoon.[citation needed]
- It continues for a few days.
- It inundates the low lying coasts.
- During high tide the run-up, water level can reach as much as 3–4 m above Maximum Water Level (MWL).
See also
[edit]References
[edit]- ^ Jansà, Agusti; Ramis, Climent (2021). "The Balearic rissaga: from pioneering research to present-day knowledge". Natural Hazards. 106 (2): 1269–1297. Bibcode:2021NatHa.106.1269J. doi:10.1007/s11069-020-04221-3. ISSN 0921-030X.
- ^ Remya P G, S Vishnu, B Praveen Kumar, T M Balakrishnan Nair, B Rohith (2016). "Tele-connection between the North Indian Ocean high swell events and Meteorological Conditions over the Southern Indian Ocean". Journal of Geophysical Research: Oceans. 121 (10): 7476–7494. Bibcode:2016JGRC..121.7476R. doi:10.1002/2016JC011723.
{{cite journal}}: CS1 maint: multiple names: authors list (link) - ^ a b Swathy Krishna, P. S.; Sheela Nair, L.; Ramesh, M. (2023), Jayaraju, N.; Sreenivasulu, G.; Madakka, M.; Manjulatha, M. (eds.), "Coastal Flooding in India: An Overview", Coasts, Estuaries and Lakes, Cham: Springer International Publishing, pp. 25–37, doi:10.1007/978-3-031-21644-2_2, ISBN 978-3-031-21643-5, retrieved 2024-04-05
