Titlebook: Coastline Changes of the Baltic Sea from South to East; Past and Future Proj Jan Harff,Kazimierz Furmańczyk,Hans von Storch Book 2017 Sprin

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Changes in the Szczecin Lagoon Shoreline as Determined from Selected Seventeenth and Nineteenth Centułomino showed a 200–700 m change to have occurred between 1695 and 1886. In addition, depths of the Szczecin Lagoon in 1755 and 1886 were compared and other map components that supported the hypothesis were indicated. A comparison of the Płocin Cove on four maps from the seventeenth century was bee

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Retrieving the Signal of Climate Change from Numerically Simulated Sediment Transport Along the East90 but behaves substantially different since then. The simulated bulk potential sediment transport along the Curonian Spit and along the entire eastern coast of the sea (incl. the Gulf of Riga) gradually increases during the entire simulation interval but the net transport reveals a decrease from th

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Sea-Level Change and Flood Risks at Estonian Coastal Zonethe twenty-first century. A significant coastal flooding risk affects four cities, Pärnu, Kuressaare, Haapsalu and Tallinn and eight smaller towns. The largest coastal flooding in Estonia is recorded in Pärnu, with the highest sea level 275 cm in 2005. Calculations show that due to the impact of pre

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2211-0577 t of modern climate change. This anthology comprises the results of the research project “Coastline Changes of the southern Baltic Sea – Past and future projection (CoPaF)” funded by the Polish Ministry of Scie978-3-319-84266-0978-3-319-49894-2Series ISSN 2211-0577 Series E-ISSN 2211-0585

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K. Manjunath Kamath,R. Sanjeev Kunteticular where eustatic sea-level rise is superimposed on isostatic subsidence and storm induced coastal erosion. This is the case on the southern and eastern Baltic Sea coast. In the South, glacio-isostatic subsidence enhances the effect of climate induced sea-level rise and strong storm effects cau

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