Environmental Science: An Indian Journal
ISSN (PRINT):0974-7451

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 Ivan, a solid Category 4 tropical storm (downsized to a Category 3 at landfall), caused across the board disintegration and overwash along the northwestern Florida obstruction island sea shores. This examination analyzes the tempest effect and momentary post-storm recuperation along a 200-km stretch of coast from Fort Walton Beach eastbound to St. George Island. One prestorm and three poststorm sea shore profile overviews were led to measure the tempest prompted morphological changes and poststorm recuperation. Forty-six channels were exhumed to examine the qualities and thickness of subaerial storm stores. Broad immersion and overwash happened inside 100 km from the tempest community at landfall. Noteworthy sea shore/rise disintegration was estimated similarly as 300 km east of the tempest place. The most elevated height of sea shore disintegration expanded impressively over the deliberate tempest flood level, demonstrating that storm-wave arrangement and swash run-up assumed noteworthy jobs in controlling the rise of sea shore disintegration. A basic experimental recipe repeated the wave arrangement and swash run-up sensibly well. Sea shore recuperation started following the tempest. Inside 90 days, the embankment peak recuperated to its prestorm height, in spite of the fact that it was presently found roughly 15 m landward for nonoverwashed locales and 30 to 40 m for overwashed destinations. The precarious prestorm foreshore slant was reestablished from the delicate tempest profile inside 30 days.

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Citations : 543

Environmental Science: An Indian Journal received 543 citations as per Google Scholar report

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