![]() Tauktae continued intensifying into May 15, reaching severe cyclonic storm status later that day. The storm soon took a northward turn, continuing to gradually intensify because of warm waters near the coast, and the system strengthened into a cyclonic storm and was named Tauktae later that same day. The low drifted eastward and organized into a deep depression by May 14. ![]() The second depression, first cyclonic storm, first severe cyclonic storm, first very severe cyclonic storm, and first extremely severe cyclonic storm of the 2021 North Indian Ocean cyclone season, Tauktae originated from an area of low pressure in the Arabian Sea, which was first monitored by the India Meteorological Department on May 13. Part of the 2021 North Indian Ocean cyclone seasonĮxtremely Severe Cyclonic Storm Tauktae ( Burmese pronunciation: ) was a powerful, deadly and damaging tropical cyclone in the Arabian Sea that became the strongest tropical cyclone to make landfall in the Indian state of Gujarat since the 1998 Gujarat cyclone and one of the strongest tropical cyclones to ever affect the west coast of India. India ( Dadra and Nagar Haveli and Daman and Diu, Goa, Gujarat, Karnataka, Kerala, Lakshadweep, Maharashtra, Delhi, Rajasthan, Haryana), Maldives, Pakistan ( Sindh), Sri Lanka London: Methuen.Cyclone Tauktae near peak intensity approaching Gujarat in India on May 17 Tsoar H (1994) Bagnold, RA 1941: The physics of blown sand and desert dunes. ![]() Suanez S, Cariolet JM, Cancouët R, Ardhuin F, Delacourt C (2012) Dune recovery after storm erosion on a high-energy beach: Vougeot Beach, Brittany (France). Priestas AM, Fagherazzi S (2010) Morphological barrier island changes and recovery of dunes after Hurricane Dennis, St. Murty CS, Veerayya M, Varadachari VVR (1982) Morphological changes of the beaches of Goa Moulton MA, Hesp PA, da Silva GM, Keane R, Fernandez GB (2021) Surfzone-beach-dune interactions along a variable low wave energy dissipative beach. Kumar KV, Aboobacker VM, Saheed PP, Vethamony P (2012) Coastal circulation along the central west coast of India during cyclone Phyan: measurements and numerical simulations. Ganesan P, Gaonkar SS (2006) Seasonal beach profiling along Malvan and Kotharwadi coast, southern Maharashtra, central west coast of India. Ocean Eng 227:108880ĭora GU, SanilKumar V, Philip CS, Johnson G (2014) Observation on foreshore morphodynamics of microtidal sandy beaches KeywordsĪravind P, Amrutha MM, Kumar VS (2021) Ocean wave dynamics in the coastal area of the central west coast of India and its variability. The cyclone impact on the beach profiles in terms of changes in morphology features and beach volumes is presented in this paper. Further measurements of monthly profiles are carried out. within one month of the cyclone passage, showed varying rates of accretion/erosion. Profiles measured between 8 and 27 June, i.e. The retreat of the berm was between 5 and 16 m, while the foreshore erosion volumes ranged between 25.82 and 132.5 m 3/m. The cyclone waves and wind impact on the beaches resulted in erosion at most locations. Beach profiles at 9 locations were measured before and after the cyclone, and volumes on the foreshore were compared. A total coastal stretch of about 27 km long in South Goa and 7 km in North Goa is considered. ![]() The influence of the Tauktae cyclone on beach morphology has been studied in this paper. ![]() The effect of this cyclone was felt severely along the coastal stretches due to increased wave and wind effects over the beaches. The cyclone passed along the Goa coast on, wherein the eye of the cyclone was about 100 km from the coastline. Extremely severe cyclonic storm Tauktae traversed along the west coast of India during 14– and reached its peak on. ![]()
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