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本文介绍一种求解涡度流函数形式的定常不可压缩Navier-Stokes方程的半隐式指数型差分格式。涡度方程用上述格式求解,而流函数方程用多层网格法求解。这种组合求解方式具有很好的稳定性及较快的收敛速度。本文对Re=100,400,1000,3000,5000的驱动方腔及Re=400,1000的驱动长方腔进行了数值模拟,结果与现有的计算相吻合。 相似文献
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Brian A. Tinsley 《Advances in Space Research (includes Cospar's Information Bulletin, Space Research Today)》2012
This paper outlines, and explores the uncertainties in, hypothesized connections between a series of processes that could explain two long-standing puzzles; those of (1) the observed winter storm vorticity responses to atmospheric energy inputs that change the ionosphere–earth current density, Jz, that appear to involve storm invigoration, and (2) changes in anti-cyclonic blocking and circulation that include the observed colder winters in Great Britain and western Europe at solar minima, and especially at extended solar minima. A working hypothesis for the mechanism responsible for (1) is that the flow of Jz through conductivity gradients, as in stratified cloud layers and fog, especially with sea-salt aerosol haze over the high latitude winter oceans, deposits electric changes on droplets and aerosol particles; most importantly on cloud condensation nuclei (CCN). These electric charges modulate scavenging of the particles in clouds and haze layers, increasing the concentration of small CCN and decreasing the concentration of large CCN. When further cloud formation occurs there is increased concentration of small droplets and decreased concentration of large ones, reducing coalescence and the production of rain. Thus updrafts carry more liquid water above the freezing level, and there the increased production of ice releases more latent heat and invigorates the updraft (the Rosenfeld mechanism), leading to increased vorticity. Here we explore the major uncertainties for the reality of the above chain of physical processes. A consequence of cumulative cyclonic vorticity increases is increases in downstream anti-cyclonic blocking. A further working hypothesis for (2) is that the invigoration may be large enough to contribute to the observed increases in blocking in winters at solar minima (high Jz) in the North Atlantic, that result in colder winters in the UK and northern Europe. 相似文献
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在保证面积不变的情况下,选取不同的长轴、短轴,对波瓣混合器进行椭圆形切扇修形,研究切口深度与宽度对波瓣混合器掺混性能的影响规律。使用商用 CFD 软件对流场进行数值模拟。结果显示,对波瓣侧壁进行切扇处理会加强流向涡的强度,切扇越深,流向涡强度越大;切扇波瓣流向涡的耗散速率要大于基准波瓣混合器的流向涡耗散速率,预示着更为高效的掺混;引射系数与切口深度成正比,而总压恢复系数与切口深度成反比。考察了两种衡量热混合效率的模型并对其信度进行了比较,发现在 x =0.4 m 之前切扇可以提高热混合效率,而在 x =0.4 m 之后,基准波瓣混合器热混合效率要大于切扇波瓣混合器。 相似文献
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Zhu Jiang Abimael F D Loula Laboratório Nacional de Computaco Científica MCT Av Getúlio Vargas Petrópolis RJ Brazil 《南京航空航天大学学报(英文版)》2001,18(Z1)
INTRODUCTIONThe stationary incompressible Navier- Stokesequations in the primitive variables( velocity uand pressure p)- vΔu + u . u + p =f . u =0u =g inΩinΩonΓ( 1 )whereΩ is a set of R2 ,Γ its boundary,v thekinematic viscosity of the fluid,f a field of givenbody forces,and g a given field defined onΓ sa-tisfying the global conservation property∫Γg . n =0 ( 2 )n denotes the unit outer normal vector toΓ.The vorticity- velocity system of Eq.( 1 ) ,byintroducing the vorticityω… 相似文献
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蛇形进气道涡控设计研究 总被引:3,自引:0,他引:3
针对传统概念设计的蛇形进气道畸变大、总压恢复系数较低以及相应流场控制技术存在局限性等缺点,对典型蛇形进气道内通道二次流的涡动力学形成及其对气流分离影响分析的基础上,提出了蛇形进气道涡控设计概念,并利用数值仿真进行了初步验证.仿真结果表明:与原型方案相比,蛇形进气道涡控设计方案成功抑制了上壁面大范围的气流分离,巡航状态畸... 相似文献
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本文利用涡量-流函数法系统地研究了扇环形截面弯曲管道内的二次流动,计算结果表明了采用控制体积积分法对涡量-流函数方程进行离散来求解弯曲管道内粘性流动问题是成功的,这样可以避免对压力项的处理;对所得结果的分析揭示了该二次流动不仅受雷诺数和曲率影响,而且扇形中心角、内外径之比对该流动的影响也是显著的。 相似文献
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Brian A. Tinsley Limin Zhou Weiping Liu 《Advances in Space Research (includes Cospar's Information Bulletin, Space Research Today)》2012
Small changes in the vorticity of winter storms, responding to solar wind variations, are found in winters from 1957 to 2011, and are greater for winters with higher levels of stratospheric volcanic aerosols. Using 1993–2011 data, the response of the vorticity area index (VAI) is shown to be of larger amplitude when the days of minima in the relativistic electron flux (REF) precipitating from the radiation belts are used, instead of heliospheric current sheet (HCS) crossings, as key days in superposed epoch analyses. The HCS crossings mostly occur within a few days of the REF minima. The VAI is an objective measure of the area of high cyclonic vorticity, and for the present work is derived from ERA-40 and ERA-Interim reanalyses of global meteorological data. The VAI dependencies on the stratospheric aerosol content (SAC) and the REF are consistent with a model in which the ionosphere-earth current density (Jz) affects cloud microphysics. One of the ways in which Jz is modulated is by changes in stratospheric column resistance (S), which is increased by stratospheric aerosols. Because S is in series with the tropospheric column resistance (T), Jz modulation by REF requires that S be not negligible with respect to T. So the Jz modulation and the VAI response appear when the SAC is very high, or the REF reductions (which also increase S) are very deep, and when the product of the SAC and the reciprocal of the REF exceeds a threshold value dependent on T. 相似文献