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Climate Change Impacts on Cities in the Baltic Sea Region  

Sonja Deppisch

While not all projected climate change impacts are affecting especially and directly at all the cities of the Baltic Sea region (bsr), including its basin, those cities expect very different direct as well as indirect impacts of climate change. The impacts are also a matter of location, if the city with its built structures and concentration of population is located in the northern or southern part of this basin, or more inland or directly at the coast. As there are many different definitions in use trying to determine what a city is, also in the different national contexts of the bsr, here it is cities in the sense of being human-dominated densely populated areas, which are also characterized by higher concentrations of built-up areas, infrastructure, and soil-sealing as well as socioeconomic roles than rural settlements are. Those characteristics render cities also especially vulnerable to climate change impacts while there are some opportunities arising too. There are many studies on climate change impacts on the Baltic Sea itself as well as on the various ecosystems, but the studies on the observed as well as potential future impacts of climate change on cities are disperse, many are also of a national character or concentrating on a small number of cases, leaving some cities not well studied at all. This renders an all-encompassing picture on the cities within the bsr difficult and even more complicated as every city provides a mix of built-up and open structures, of socioeconomic structure and role in a region, nation-state, or even on an international level, and further characteristics. Their urban development is dependent on manifold various interdependencies as well as climatic and nonclimatic drivers, such as, to name just a few diverse examples, urban to international governance processes, or topography and location, or also different socioeconomic vulnerabilities within the Baltic Sea basin. Accordingly every urban society and structure provides specific exposure, vulnerabilities, and adaptive capacity. Generally, the cities of the bsr have to deal with the impacts of temperature rise, natural hazards, and extreme events, and, depending on location and topography, with sea-level rise. With reference to temperature rise and the increase of heat waves, it is important to consider that cities of a certain size within the Baltic Sea basin contribute to their own urban climatic conditions and provide already urban heat islands. Also, urban planning and building facilitated by local political decisions contribute to the extent of urban floods as well as their damage, as these are regulating, for example, the sealing of soils or new built-up areas in flood-prone zones.

Article

Two Millennia of Natural and Anthropogenic Changes of the Polish Baltic Coast  

Andrzej Osadczuk, Ryszard Krzysztof Borówka, and Joanna Dudzińska-Nowak

Changes of the coast are a net result of morphodynamic processes driven by changes in external conditions. Morphodynamics can be understood as feedback between shore topography and hydrodynamics, the latter including bedload transport, which alters the morphology of the coast. The evolution of a marine coast can take various pathways depending on the time scale, shoreline length, geological setting, tectonic underpinnings, type and availability of sediments in the nearshore zone, sea level changes, intensity of waves and currents, and the influence of the adjacent land masses. A spatio-temporal approach (processes of millennial, decadal, annual, and seasonal change) is particularly important for coastal areas built of erosion-prone, poorly consolidated glacial and postglacial deposits. This is the case of the southern Baltic Sea coast where the shore has been and continues to be impacted by geological processes, climatic factors, and anthropogenic activities. The processes involved are shaped primarily by external factors such as wind–wave action, currents, storm surges, precipitation, winter ice cover, and gravitational mass movements. The shoreline response to climate change depends on both the nature of the change and the coastal zone characteristics. Long-term climate changes result in sea level changes. The sea level rise resulting from global warming enhances coastal erosion, particularly where the shore is built by poorly consolidated rocks and deposits. Coastal zones are usually very sensitive to all the external forces, therefore climate change will most likely be the strongest driver and will be the first to impinge on the coast, whereas the most distant changes in the oceans may produce effects delayed by decades or even centuries.