By Malvin Bjorøy, P.B. Hall
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Additional resources for [Article] A Rich Middle Triassic Source Rock in the Barents Sea Area
Comput. Phys. 227(6), 3089 (2008). 027 16. T. Chow, Open Channel Hydraulics (McGraw-Hill, 1959) 17. L. George, Finite volume methods and adaptive refinement for tsunami propagation and inundation. D. thesis, University of Washington (2006) 18. L. George, Int. J. Numer. Meth. Fluids 66(8), 939 (2011). 2298 19. E. Green, P. Naghdi, Journal of Fluid Mech. 78, 237 (1976) 20. K. G. Zhou, Int. J. Numer. Meth. Fluids 28, 541 (1998) 21. Z. Li, B. Johns, Int. J. Numer. Meth. Fluids 35, 299 (2001) 22. J.
Not only do mathematical models of these flows present the standard difficulties common to hyperbolic systems, they also require specialized techniques specific to free-surface flows over topography and multiscale resolution. Despite these challenges, it is possible to design algorithms that can effectively and efficiently simulate a range of free-surface flows. Acknowledgements The work described in this paper has resulted from an active collaboration of researchers in mathematics, computer science, and the geosciences.
L. George hyperbolic with a simple analytically known eigenstructure. Because pressure is not a conserved quantity, the system has nonconservative products that must be handled numerically (described briefly in Sect. 3). 4 Hybrid Models Some geophysical applications contain multiple interacting flow phenomena, each of which can be described by a distinct depth-averaged model. Hybrid models formed by coupling together individual depth-averaged equations are sometimes used for these applications.
[Article] A Rich Middle Triassic Source Rock in the Barents Sea Area by Malvin Bjorøy, P.B. Hall