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Materials and Methods: A Framework for the Coastal Morphodynamics

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Part of the book series: SpringerBriefs in Geography ((BRIEFSGEOGRAPHY))

Abstract

Coastal morphodynamics deal with the modification of the nearshore bottom topography shoreline shifting and beach morphology of the coastal areas through hydrodynamic, fluvial, aeolian and terrestrial processes. Nearshore ocean bottom morphological changes and consequence series of alteration dynamics are concerning the movement of sediment. To analyse the shoreline dynamics, we go over the changes in the recent positions of the shoreline of the Balasore coast for the 38 years from 1975 through 2013. Transects wise shoreline data base of Balasore coast, Odisha, India were developed for approximately 67 km of shoreline and erosional/accretional scenario has also been analysed by delineating the shoreline from Landsat imageries of 1975, 1980, 1990, 1995, 2000, 2005, 2010 and 2013. A simple linear regression model and End Point Rate (EPR) has been adopted to take out the rate of change of shoreline and its future positions based on empirical observations at 67 transects along the Balasore coast. The rate of shoreline movement calculated from the fixed base line to shoreline position of 1975, 1980, 1990, 1995, 2000, 2005 and 2010 were applied and based on this, the estimated shoreline of 2013 was calculated. The shoreline data were integrated for long- (about 17 years) and short-term (about 7 years) shift rates analysis to comprehend the shoreline change and prediction. For the prediction of future shoreline, the model has been validated with ‘t’ test followed by the comparison with present shoreline position (2013). Root Mean Square Error has also been implemented to distribute the model generated error among all transects. The present study also deals with beach morphodynamics using some numerical model. Firstly the wave propagation has been estimated by the help of Karkby and Dalrym model (1985). After analyzing the wave characteristic current characteristics can be assessed by the help of Navier and Slokes equation. After knowing the both wave and current characteristics sediment transport of near shore has been anticipated using Bailard and Soulsby model to detect the beach morphology because beach morphology is directly depends on near shore sediment dynamics.

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Correspondence to Nilay Kanti Barman .

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Barman, N.K., Chatterjee, S., Paul, A.K. (2016). Materials and Methods: A Framework for the Coastal Morphodynamics. In: Coastal Morphodynamics. SpringerBriefs in Geography. Springer, Cham. https://doi.org/10.1007/978-3-319-33575-9_3

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