Comparisons of One-way Nesting Schemes by

Q4 Earth and Planetary Sciences Papers in Meteorology and Geophysics Pub Date : 2012-01-01 DOI:10.2467/mripapers1950.29.3_125
Shoin Yagi, Yasusi Okamura
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Abstract

Various one-way nesting techniques so far presented are tested in order to decide the best technique from a practical standpoint. Nesting schemes tested here are : (1) Schemes with special care to avoid over-specification as a boundary value problem. i) The scheme with simple extrapolation (referred to as SE-scheme) ii) The scheme of SundstrOm (1973) (SS-scheme) iii) The scheme modified by taking account of gradient value of coarse mesh model in extrapolation (SG-scheme) iv) The scheme of Okamura (1975) (SO-cheme) (2) The scheme of Orlanski (1976) with Sommerfeld's radiation condition (0-scheme) (3) The scheme of Perkey & Kreizberg (1976) in which the tendency is smoothed in the lateral boundary layer (T-scheme) (4) The scheme with Newtonian damping in the lateral boundary layer i) Davies' method (1976) (D1-scheme) ii) The scheme utilizing simple Newtonian damping (Do-scheme) Numerical tests for comparison are done under the following conditions : (1) Tests in which the phase velocity error is given in the outer domain during the forecasting period. (Test 1) (2) Tests in which isolated disturbance is given in the inner fine mesh domain at intial time. (Test 2) Results of the test are as follows : (1) T-scheme is the best one because of its least deviation from the control run and the computationally stable results. (2) Dr-scheme and Do-scheme are the second best. Little difference is found between the results of the two schemes. Damping coefficient used in these tests seems to cause more error than in T-scheme because of its inadequately large value. (3) Among the SE-, SS-, SO-, o-, and SG-schemes, SG-scheme gives the least error. The error in that scheme is the same order as that in D1-scheme within 24 hours forecast. But, for longer time integration,, the results of SG-scheme tend to be unstable. (4) When 0-scheme is adopted, results are very sensitive to the way in which the phase velocity of the disturbances near the boundary is estimated. 126S. Yagi and Y. OkamuraVol. 29, No. 3
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单向嵌套方案的比较
为了从实用的角度决定最佳的技术,我们测试了目前提出的各种单向嵌套技术。这里测试的嵌套方案有:(1)特别注意避免作为边界值问题的过度规范的方案。i)简单外推方案(简称se方案)ii) SundstrOm(1973)方案(ss方案)iii)外推中考虑粗网格模型梯度值修正的方案(sg方案)iv) Okamura(1975)方案(so方案)(2)Orlanski(1976)在Sommerfeld辐射条件下的方案(0方案)(3)Perkey & Kreizberg(1976)在侧边界层中平滑趋势的方案(t方案)(4)牛顿方案横向边界层阻尼i) Davies方法(1976)(d1格式)ii)利用简单牛顿阻尼(do格式)的方案在下列条件下进行了比较的数值试验:(1)在预测期间在外域给出相速度误差的试验。(试验1)(试验2)初始时刻在内细网格域中给出孤立扰动的试验。(试验2)试验结果如下:(1)t方案与控制运行偏差最小,计算结果稳定,是最佳方案。(2) Dr-scheme和Do-scheme次之。两种方案的结果差别不大。在这些试验中使用的阻尼系数由于其值不够大,似乎比t型方案产生更大的误差。(3)在SE-、SS-、SO-、o-和sg - 4种格式中,sg -格式误差最小。该方案在24小时预报范围内的误差与d1方案相同数量级。但是,对于较长时间的积分,SG-scheme的结果往往不稳定。(4)当采用0格式时,结果对边界附近扰动相速度的估计方式非常敏感。126年代。Yagi和Y. OkamuraVol。29, No. 3
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Papers in Meteorology and Geophysics
Papers in Meteorology and Geophysics Earth and Planetary Sciences-Geophysics
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