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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Introduction,e projection of coastal developments in front of the modern climate change. The anthology comprises results of a research project “Coastline Changes of the southern Baltic Sea – Past and future projection (CoPaF)” which was run by a team of Estonian, German, and Polish geoscientists and coastal engi

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What Determines the Change of Coastlines in the Baltic Sea?l water level, meteorological, and GPS data are combined with analytical methods to solve the sea-level equation. In the result, the pattern of vertical crustal movement can be displayed as maps covering the uplifting Fennoscandian Shield and its subsiding belt. Whereas along the uplifting coasts mo

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Factors and Processes Forming the Polish Southern Baltic Sea Coast on Various Temporal and Spatial S acting simultaneously on different levels, overlap, causing a complex contemporary picture of the processes and forms. Spatial and temporal differentiation of structures and processes are to be considered in the Southern Baltic Sea for modelling approaches of coastal changes.

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The Dynamic Equilibrium Shore Model for the Reconstruction and Future Projection of Coastal Morphodyale. The DESM model requires data of historical coastline configuration derived from maps, a high-resolution modern Digital Elevation Model (DEM), relative sea-level change data, and modelling data of long-shore sediment transport capacity. This model is applied in the study to three research areas

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Modelling of Medium-Term (Decadal) Coastal Foredune Morphodynamics- Historical Hindcast and Future Sfuture projection of the same area to 2050 AD based on three different climate change scenarios. The climate change scenarios represent three different impact levels with regard to their capacity to shape the coastal morphology. Simulation results demonstrate a remarkable variability in foredune dev

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Constraints of Radiocarbon Dating in Southeastern Baltic Lagoons: Assessing the Vital Effectsthe uncertainty of reservoir effect added a considerable error to the .C ages. Moreover, fossil molluscs of the same species extracted from boreholes and outcrops yield significantly younger ages (up to several millennia) than the enclosing sediments. Both of these trends – aging and rejuvenation –

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Late Glacial to Holocene Environmental Changes (with Particular Reference to Salinity) in the Southesalinities between 6.000 and 5.000 cal. BP was not observed in our records. It is likely that this indicates the buffering of the Baltic waters from freshwaters from the south, and demonstrates the importance of terrestrial-hydrological processes for determining the long-term stability of the salini

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Morphodynamic Processes of the Swina Gate Coastal Zone Development (Southern Baltic Sea)anges were distinctly smaller. For the periods 1938–1951 and 1996–2012, when the magnitude of growths in the DBL is bigger than 2 m/year, a correlation between DBL changes in relation to the coastline exposure, beach width, DBL elevation and beach slope is clearly visible. The greatest growths in th

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