column, as well as sedimentary structures on and beneath the seafloor. Parallel to data acquisitionat sea, seismic and georadar measurements will be carried out on land for comprehensivereconstructions of shoreline change. <strong>The</strong>se combined results will provide the input necessary forthe development of multidisciplinary strategies for coastal risk assessment and will form the basisfor numerical model development.An improved understanding of the dynamics which control near-shore sediment budgets duringsea-level fluctuations is required to accurately assess future coastal evolution. Data concerningthese processes on variable timescales are needed to assess the conditions which trigger coastalhazards. By considering various scenarios for climate change and human intervention which affectSLR and shoreline migration, the following key and interrelated topics will be addressed in aninnovative change analysis approach: (1) changes in near-shore slope gradients; (2) changes innear-shore circulation systems; (3) impacts on the coastal sediment budget, including rates of andbalances between erosion and sedimentation; (4) effects on biological and ecological systems; and(5) disturbances of coastal infrastructures.Principal research targets are primarily changing river-mouth systems, in particular: (1) thetransition from deltaic to estuarine systems; (2) shoreline changes ranging from prograding toretrograding; (3) inland migration of the groundwater/saltwater interface which leads to the pollutionof freshwater resources; and (4) the consequences of sand/gravel extraction and waste dumping.In addition to direct connections with B5(2), B5(1) will have close ties to A4 (climate change), B1(nursery habitats in the coastal zone), B4 (impacts of deep-sea hazards) and B6 (juridicaldefinitions of offshore economic zones). Research platforms P1, P2 and P4 will be usedextensively.5. ReferencesCaldas LH, Stattegger K, Vital H (2006) Holocene sea-level history: Evidence from coastalsediments of the northern Rio Grande do Norte coast, NE Brazil. Marine Geology 228, 39-53.Church JA, White NJ (2006) A 20th century acceleration in global sea-level rise. GeophysicalResearch Letters 33, L01602, doi:10.1029/2005GL024826.Crossland JC, Kremer HH, Lindeboom HJ, Marshall Crossland JI, Le Tissier MD (2005) CoastalFluxes in the Anthropocene. Global Change – <strong>The</strong> IGBP Series, 232 pp., Springer.Diesing M, Kubicki A, Winter C, Schwarzer K (in press) Decadal scale stability of sorted bedforms,German Bight, southeastern North Sea. Continental Shelf Research.Ericson JP, Vörösmarty CJ, Dingman SL, Ward LG, Meybeck M (2006) Effective sea-level rise anddeltas: Causes of change and human dimension implications. Global and Planetary Change50, 63-82.Hanebuth T, Stattegger K, Grootes P (2000) Rapid flooding of the Sunda Shelf - a late glacialsea-level record. Science 288, 1033-1035.Overpeck JT, Otto-Bliesner BL, Miller GH, Muhs DR, Alley RB, Kiehl JT (2006) Paleoclimaticevidence for future ice-sheet instability and rapid sea-level rise. Science 311, 1747-1750.83
Pickrill RA, Todd BJ (2003) <strong>The</strong> multiple roles of acoustic mapping in integrated oceanmanagement, Canadian Atlantic continental margin. <strong>Ocean</strong> & Coastal Management 46,601-614.Rabbel W (2006) Seismic methods for hydro-geological applications. In: R Kirsch (ed.),Hydrogeophysics, Springer, Berlin, 23-84.Schwarzer K, Diesing M, Larson M, Niedermeyer R-O, Schumacher W, Furmanczyk K (2003)Coastline evolution at different time scales. - Examples from the southern Baltic Sea(Pomeranian Bight). Marine Geology 194, 79 - 101.Syvitski JPM, Vörösmarti CJ, Kettner AJ, Green P (2005) Impact of humans on the flux ofterrestrial sediment to the global coastal ocean. Science 308, 376-380.B5(2): From Coastal Hazards and Vulnerability to Risk Management2. State-of-the-artSince the IPCC’s (Intergovernmental Panel on Climate Change) first predictions of climate changeand accelerated SLR, a number of studies have addressed the issue of hazards to low-lyingcoastal areas. Several methods for the quantitative assessment of coastal vulnerability have beenproposed (e.g. Boruff et al. 2005, Klein and Nicholls 1999). <strong>The</strong>se methods primarily analyze theeffects of gradual coastal-system changes, such as slow inundation, erosion or saltwater influenceon groundwater and soils. More recently, coastal risk research has focused on eithermacroeconomic assessment models on a global scale (Vafeidis et al. 2004) or on specific regional(microscale) aspects of the economic drawbacks arising from SLR (Darwin and Tol 2001). In 2004and 2005, devastating flood events revealed that vulnerability assessments which rely solely onmorphologic or economic methods are not adequate to support the complex process of coastal riskmitigation. Hence, a comprehensive approach for risk modeling which also incorporates social andecological components is needed. <strong>The</strong> first attempts to derive integrated decision-making supporttools for flood risk assessment and management are underway (Onate and Piazzese 2005), butthey need to be further expanded to include multihazard situations as well as various types ofcoastal environments and regions.3. Previous and on-going work of the proponentsH. Sterr has been a member of the Coastal Zone Management Subgroup of the IPCC and areviewing author of the IPCC Second Assessment Report. He has directed several researchprojects on coastal hazards related to climate change which have focused on: (a) the developmentof risk assessment methods on various spatial scales (Sterr et al. 2003); (b) scenario-basedmodeling of vulnerability via GIS (Sylt Island, State of Para, Brazil), and (c) risk management in theNorth Sea region and Europe (COMRISK, FLOODSITE, EU). U. Schmidt from the Department ofEconomics of the University of Kiel has conducted several research projects in the area of riskperception, risk evaluation and risk management (Schmidt and Zank 2005). W. Dombrowsky fromthe Disaster Research Unit at the University of Kiel has conducted several projects on disaster andflood management (Dombrowsky and Ohlendieck 1998). R. Horn is a renowned specialist on soil84
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1 General Information about the Clu
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ITQ’sISAISOSJRGKCMSKitzLALIFLIMSL
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WTOWTSHXAFSXRDZMBWorld Trade Organi
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Prof. Dr. Boris Culik • Maritimes
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GMT-Geschäf*sstelleWe"*w{eltJ"*n $
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f,rylheonRaytheon Anschütz GmbHPos