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Titlebook: Computerized Modeling of Sedimentary Systems; Jan Harff,Wolfram Lemke,Karl Stattegger Conference proceedings 1999 Springer-Verlag Berlin H

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asured data and the dynamics of sedimentary systems. Complex interaction of environmental factors with natural variations and increasing anthropogenic intervention is reflected in the sedimentary record at varying scales. The understanding of these processes gives way to the reconstruction of the pa
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SEDLOB and PATLOB: Two Numerical Tools for Modeling Climatically-Forced Sediment and Water Volume Trg alluvial or deltaic basin fill (cf. Bitzer and Pflug 1989; Cao and Lerche 1994; Paola et al. 1992; Slingerland et al. 1994; Syvitzki and Daughney 1992; Tetzlaff and Harbaugh 1989). In order to simulate large basins we need to couple an ocean general circulation model (OGCM) with an sedimentation model.
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Field and Numerical Studies of Near-Bed Aggregate Dynamicsally investigated (Rouse 1937). Only recently have biologists become interested in the water mass above the sediment-water interface. However, the dynamics of particles, their interaction and modification within the last few meters above the seafloor (the benthic boundary layer — BBL) is in many terms poorly understood.
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Conference proceedings 1999ly in cases where observations are limited and/or expensive, computer simulations may substitute for the lack of data. State-of-the-art research work requires a thorough knowledge of processes at the interfaces between atmosphere, hydrosphere, biosphere, and lithosphere, and is therefore an interdisciplinary approach.
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Aftermath: Napoleon and Beyond,to the Oder Estuary, which forms the border between Germany and Poland. The concentration levels are clearly related to the higher waves and water depth. The model results agree with known values and data images in the Oder Estuary.
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W.-Y. Hsiang,S. Kobayashi,A. Weinsteinn as a result of the study of complicated geological objects. Additionally, tools of formal logic, modern mathematical logic [2, 6] and computer processing of data [3, 4] are also employed for the simulation and detection of CE relations.
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