Titlebook: Broad Scale Coastal Simulation; New Techniques to Un Robert J. Nicholls,Richard J. Dawson,Sophie A. Day Book 2015 Springer Science+Business

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Johan Jansson,Agneta Marell,Annika Nordlundress this challenge, presenting the visualisation methods that have been developed to assist in the communication of the Tyndall Coastal Simulator’s output. These methods range from relatively low-cost landscape visualisation tools underpinned by expert judgement and simple rule-based models, used t

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Chun-Ming Yang,I Ling Ling,Chih Yun Yanged significantly over the last two decades. This chapter specifically addresses the ways in which national, regional and local stakeholder interests have interacted during this tumultuous time in North Norfolk to negotiate pathways for adapting to coastal change. The case example presented in this c

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Climate Downscaling: Local Mean Sea Level, Surge and Wave Modelling,he future changes in surge and wave climate forced by winds and sea-level atmospheric pressures from a version of the Met Office Hadley Centre Climate Model (HadCM3), assuming various greenhouse gas emission scenarios and for various climate model parameter choices. The local spatial variation in me

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Broad-Scale Hydrodynamic Simulation, Wave Transformation and Sediment Pathways,o-informatics system. More precisely it is used to generate a look-up table to compute inshore waves from 1960 to 2099 taking account of the cumulative effect of climate change on atmospheric forcing and sea-level rise. Simulations take into account four scenarios of linear sea-level rise and a base

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Land Use Dynamics and Coastal Management,r different socio-economic futures. The core elements of this model are the location preferences of (changing) individual residential agents and the constraints imposed by planners through land-use policy..The MCA method is simpler than the ABM method and useful for developing and realising socio-ec

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Evaluating Broadscale Morphological Change in the Coastal Zone Using a Logic-Based Behavioural Systse (DPSIR) framework. The uncertainty in future geomorphological change is then described using likelihoods for these possible responses based on individual or consensus expert judgement captured within a simple, transparent matrix..The methodology provides a whole system level of analysis. It allow