Titlebook: Crisis on the Coast and Hinterland; Assessing India’s Ea Ashis Kumar Paul,Anurupa Paul Book 2023 The Editor(s) (if applicable) and The Auth

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Letzte Etappe – die Schatzkartents in the Bay of Bengal region. The river carries sediment outlets into the shallow sea region of the Subarnarekha estuary mouth, which is further redistributed along the shoreline by the different reworking agents like waves, tides, currents, longshore drifts, and storm surges. Depending on the sh

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Zweite Etappe – Standortbetrachtung the beach and dune sediment exchange. The established process-response models fail to predict the integral pattern of change due to the complexity of the system. Therefore, an alternate method, such as repeatedly measuring the topography with respect to a fixpoint/landmark to develop a comprehensiv

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The Framework, An Introduction, of the shoreline influences the rate of accumulation and erosion in the study area, which is classified into multiple stages of the beach dune development process. The beach stage and dune stage modelling approach is based on the mutual co-adjustment of intertidal seashore surf-zone morphology, hyd

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Zweite Etappe – Standortbetrachtungcal Asia. Due to climate change coupled with anthropogenic factors, the discharge of floodwater and sediments in the lagoon has been reduced, resulting in a low flow of water and sediments into the sea through the lagoon outlet. The longshore drift along the east coast of India is from south to nort

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Erste Etappe – Was erwartet mich?dy beach berm and a surface layer of shells. Active swash wave energy accumulated sands on the backshores and pushed them landward by repeated overwash processes during high energy marine wave environments. The storm and non-storm conditions with steeper waves and less steep long-period swell waves

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For the Conditions of An Analysisds, lagoons, embayments, beach ridges and sand dunes, spits and bars, tidal mudflats and mangroves, sandy sea beaches, and rocky headlands. They harbour a large number of flora and other organisms in the regional coastal system and act as natural buffers against the tropical storms and high energy m

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Psychologische Grundlagen der Wahrnehmung,gradation is a process that can come into action in any physiographic environment. But its type, intensity, and magnitude vary from place to place. Land degradation is caused by anthropogenic factors as well as natural phenomena in the middle and lower courses of the Subarnarekha River basin. Defore

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Theorizing Socio-Spatial Practices,d play a significant role in providing a new dimension to the river continuum concept. It is the buffer zone where vegetation acts as a filter to maintain the health of the entire riparian area. The riparian corridor includes all perennial streams with defined channel flow. It also encompasses adjac