Alopecia-Areata
发表于 2025-3-23 13:39:51
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Petechiae
发表于 2025-3-23 16:13:02
Chebyshev spectral and pseudospectral solutions of the Navier-Stokes equations,th influence matrix technique for the pressure computation is applied to the simulation of convective phenomena in liquid metals. Some results are compared with those produced by finite elements. In the second part, a pseudospectral algorithm using finite element preconditioning for the momentum equ
crease
发表于 2025-3-23 21:57:46
Analysis of strongly interacting viscous-inviscid flows including separation,curately resolving many of the details of transonic shock-wave, boundary-layer interaction. Second, the results show that the effect of displacement thickness interaction dominates over the effects produced by normal pressure gradients and imbedded shocks for transonic shock induced separated flows.
Initiative
发表于 2025-3-24 01:12:51
An improved Euler method for computing steady transonic flows,o time-dependent, split and uses a finite-volume formulation. Shock waves are captured crisply, with minimal added smoothing, by means of an operator-switching facility which more accurately reflects the direction of propagation of signals. The method is robust, versatile, and holds promise for trea
Collected
发表于 2025-3-24 04:37:31
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BALE
发表于 2025-3-24 10:17:29
J. J. Lions generation of sound in a flow field occurs at small spatial scales with high energy, while its propagation in the farfield has to be observed on a large spatial scale with only low energy. The challenge of different scales can be addressed by employing different numerical schemes in the individual
GOAT
发表于 2025-3-24 14:29:30
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欢乐中国
发表于 2025-3-24 18:31:52
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垫子
发表于 2025-3-24 19:15:18
C. A. J. Fletcherolves multiple scales. Simulating the whole domain with one solver is not feasible and out of range on todays supercomputer. Since the involving physics appear on different scales, the effects can be spatially separated into different domains. The interaction between the domains is realised with cou
煤渣
发表于 2025-3-25 00:08:20
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