期刊文献+

近海区域二阶紊流封闭模型的比较研究 被引量:2

Comparison of two-order closure model in coastal areas
下载PDF
导出
摘要 将雷诺应力方程不同封闭方式归结为稳定函数的差异,并以此作为区分标准,总结了6种国内外采用过的稳定函数并以统一的形式列出,分析不同紊流模型稳定函数的分布和影响因素,并且通过实验资料进行了比较分析,发现(1)2000年后提出的3种稳定函数得到的临界理查德森数大于2000年前的3种,更符合实际情况,这与其在压强应变相关项和浮力相关项中增加了旋转效应和重分布效应有关;(2)尽管这3种模型考虑的因素更加全面,但在某些特定场合下,如边界层,与实验的吻合程度反不如前3种较早的稳定函数,反映了封闭模型本身存在的缺陷。最后,提出了二阶紊流封闭模型还待解决的问题。 With advance of knowledge on turbulence and computer capability in recent years, two-order closure model has made new process. Different two-order closure models lead to different stability functions. Three earlier models (before 2000) and three later ones (after 2000) have been concluded in a unified form and then have been compared in the paper. After that some experimental data are compared with the model results. It is found that: (t) the later models (after 2000) obtain more realistic Richardson Number than the earlier models (before 2000) ; (2) in some particular tests, such as boundary layer, performance of earlier models is even superior to the later's, which reflects the faults of the later ones. Finally, problems to be solved are put forward.
出处 《海洋通报》 CAS CSCD 北大核心 2010年第1期12-21,共10页 Marine Science Bulletin
基金 水文水资源与水利工程科学国家重点实验室开放基金(2007491211)
关键词 二阶紊流封闭模型 垂向紊动扩散 临界理查德森数 two-order closure model vertical turbulent mixing critical Richardson Number
  • 相关文献

参考文献7

  • 1Mellor G L, Yamada T. Development of a turbulence closure model for geophysical fluid problems [J]. Rev Geophys Space Phys, 1982, 20 (4): 851-875.
  • 2Umlauf L, Burchard H. Second-order turbulence closure model for geophysical boundary layers. A review of recent work [J]. Continental shelf Research 2005, 25: 795-827.
  • 3Canuto V M, Howard A, Cheng Y, et al. Ocean turbulence. Part I : one-point closure model. Momentum and heat vertical diffusivities [J]. Journal of Physical Oceanography, 2001, 31:1 413-1 426.
  • 4Cheng Y, Canuto V M. Howard A M. An improved model for the turbulent PBL [J]. Journal of the Atmospheric Science, 2002, 59:1 550-1 565.
  • 5Rodi W. A new algebraic relation for calculating the Reynolds stresses [J]. Zeitschrift fur Angewandte Mathematic und Mechanik, 1976, 56:T219-T221.
  • 6Wang D, Large W G, McWillimas J C. Large eddy simulation of the equatorial ocean boundary layer: Diurnal cycle, eddy viscosity and horizontal rotation [J]. J Geoohvs Res. 1996. 101 (C2): 3 649-3 662.
  • 7Monin A S, Yaglom A M. Statistical Fluid Mechanics: Mechanics of Turbulence [M]. 1971: 1-769.

同被引文献20

  • 1陆永军,左利钦,王红川,李浩麟.波浪与潮流共同作用下二维泥沙数学模型[J].泥沙研究,2005,30(6):1-12. 被引量:32
  • 2KANTHA I. H, CLAYSON C A. An improved mixed layer model for geophysical applications [J].Geophys. Res. , 1994,99: 25232-5266.
  • 3ZHANG Y, BAPTISTA A M. A cross-scale model for 3D baroclinic circulation in estuary-plume shelf systems- I . Formulation and skillassessment[J].Continental Shelf Research, 2005, 25:935 -972.
  • 4宋志尧.海岸河口三维水流场垂向级数解模型[D].南京:河海大学,1999.
  • 5UMLAUF L, BURCHARD H. Second-order turbulence closure model for geophysical boundary layers--A review of recent work[J]. Continental Shelf Research, 2005, 25: 795-827.
  • 6HINZE J O. Turbulence[M]. New York: McGraw-Hill, 1975.
  • 7BLUMBERG A F, MELLOR G L. A description of a three-dimensional coastal ocean circulation model[M].//HEAPS N S. Three-Dimensional Coastal Ocean Models. Washington: American Geophysical Union,1975: 1-16.
  • 8SHIH T H, LIOU W W, SHABBIR A, et al. A new eddy viscosity model for high Reynolds number turbulence flows[J]. Model Devel opment and Validation. 1995, 24(3)227.
  • 9MELLOR G L. Development of a turbulence closure model for geophysical fluid problems[J]. Reviews of Geophysics and Space physics, 1982,20(4) : 851-875.
  • 10杨阳,周伟东,董丹鹏.大洋环流的诊断计算[J].海洋通报,2007,26(6):3-8. 被引量:4

引证文献2

二级引证文献3

相关作者

内容加载中请稍等...

相关机构

内容加载中请稍等...

相关主题

内容加载中请稍等...

浏览历史

内容加载中请稍等...
;
使用帮助 返回顶部