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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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书目名称Computerized Modeling of Sedimentary Systems
编辑Jan Harff,Wolfram Lemke,Karl Stattegger
视频video
概述Wide spectrum of application.Numerous case studies
图书封面Titlebook: Computerized Modeling of Sedimentary Systems;  Jan Harff,Wolfram Lemke,Karl Stattegger Conference proceedings 1999 Springer-Verlag Berlin H
描述Computerized modeling is a powerful tool to describe the complex interrelations between measured 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 past and is a key to the prediction of future trends. Especially 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.
出版日期Conference proceedings 1999
关键词Coast; Iceberg; Ocean; Sediment; computer simulation; marine; model; modeling; simulation
版次1
doihttps://doi.org/10.1007/978-3-662-03902-1
isbn_softcover978-3-642-08380-8
isbn_ebook978-3-662-03902-1
copyrightSpringer-Verlag Berlin Heidelberg 1999
The information of publication is updating

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Climate Cycles and Climate Transitions as a Response to Astronomical and CO2 Forcingsty and . sin . is the precessional effect, with . being the longitude of the perihelion as measured from the moving equinox. Each of the orbital parameters can be expressed as a quasi-periodic function of time. According to the astronomical theory, low summer insolation could prevent the winter snow
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Icebergs in the North Atlantic: Modelling Circulation Changes and Glacio-Marine Depositionwith a strong reduction in deepwater formation or even a breakdown of the conveyor belt (Bond 1995; Bond and Lotti 1995; Broecker 1991; Seidov et al. 1996). These changes depend on (i) the amount of freshwater brought in and (ii) the locations of freshwater input and its transport path; that means t
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SEDLOB and PATLOB: Two Numerical Tools for Modeling Climatically-Forced Sediment and Water Volume Trc circulation patterns. Most sedimentation models developed during the last decade are designed for small basins and specific sediment input simulating 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 19
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Field and Numerical Studies of Near-Bed Aggregate Dynamics and consequently their incorporation in the sediment. Early on in sedimentology, major focus was set on the size distribution of particles above the sea bed and in the sediments. The vertical distribution of different particle size classes and its relationship to the hydrodynamic regime was empiric
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