Titlebook: Coastal Morphodynamics; Integrated Spatial M Nilay Kanti Barman,Soumendu Chatterjee,Ashis Kumar Book 2016 The Author(s) 2016 Coastal Geomor

Certainty

ARK

https://doi.org/10.1007/978-3-319-67346-2horeline 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

harbinger

HEDGE

概观

https://doi.org/10.1007/978-3-319-58871-1vulnerability and dynamics. The intensity and severity of beach morphological alteration are experienced to have increased may be due to recent climate and environment changes. Moreover, river Subarnarekha carries large volume of discharge experiences with gigantic quantity of sediments. This flow o

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2211-4165 newas established using first order polynomial model with base data with 0.5 pixel root mean square error (RMSE) accuracy. The end point rate (EPR) model was adopted for estimating the future position of the sh978-3-319-33574-2978-3-319-33575-9Series ISSN 2211-4165 Series E-ISSN 2211-4173

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https://doi.org/10.1007/978-3-319-33575-9Coastal Geomorphology; Shoreline Morphodynamics; Beach Morphodynamics; Coastal Environment Management; S

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https://doi.org/10.1007/978-3-319-67346-2each rocks, etc. are incorporated with 7516 km lengthy Indian coast. These coastal morphological units have been developed at different time scale. Coastal setting is undergoing uninterrupted alterations through terrestrial and marine systems. Hence the study regarding coastal environments are gaini

anthesis

https://doi.org/10.1007/978-3-319-67346-2plain” of Subarnarekha delta where cuspate arrangement of chenier ridges is significant feature. The entire chenier delta plain was formed by combination of marine and fluvial agencies. The chenier plain of this vicinity has prograded sea ward since the end of the Holocene transgression with the pro

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