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转自《新语丝》
作者:热风
看了高的第八篇代表作谈点个人对高守亭的第八篇代表作(以下简称高文)的看法。
高文在ill-condition的处理上显然照抄了B.J.Hoskins et al (1983)和K.E.Trenberth(1986)的方法。对ill-condition的处理是广义E—P理论的重点。显然高守亭在写“论文”过程中参考了Hoskins和Trenberth的论文。可是高在其“论文”的参考文献中并没有列出这些人的名字。高要是说当时没看过这些人的论文,我真是无语了,不过打死我也不相信高没看过。要不信把高的这篇论文寄给Hoskins和Trenberth看看,看他们怎么说!
比如说,高文得到的关键式第60式,是一个2维的F向量,而K.E.Trenberth(1986)的E向量(式A12)是3维的。把E向量简化成2维的就是高的F向量,虽然需要进行一点坐标变换。
本人由于比较忙没时间对高文的推导过有一一地对比,如果你要是有兴趣把它同K.E.Trenberth(1986)和B.J.Hoskins (1983)的论文仔细地对比一下,也许有更多的发现。
对E-P通量的广义发展其主要的问题就是高文所谓对ill-condition的处理,这项工作主要是由B.J.Hoskins et al (1983),K.E.Trenberth(1986)和R.A.Plumb(1985,1986)完成的,高文发表在1990年,高如果说写论文时没参考过
以上这些作者的论文,那么我就只好真的无语了!
参考文献
Hoskins, B. J., I. N. James, and G. H. White, 1983: The shape, propagation and mean-flow
interaction of large-scale weather system. J. Atmos. Sci., 40, 1595-1612.
Plumb, R. A., 1985: On the three-dimensional propagation of stationary waves. J. Atmos.
Sci., 42, 217-229.
———, 1985: An alternative form of Andrews’ conservation law for quasi-geostrophic waves
on a steady,nonuniform flow. J.Atmos.Sci., 42, 298-300.
———, 1986: Three-dimensional propagation of transient quasi-geostrophic eddies and its
relationship with the eddy forcing of the time-mean flow, J. Atmos. Sci., 43, 1657-1678.
Takaya, K., and H. Nakamura, 1997: A formulation of a wave-activity flux for stationary
Rossby waves on a zonally varying basic flow. Geophys. Res. Lett., 24, 2985-2988.
Trenberth, K. E., 1986: An assessment of the impact of transient eddies on the zonal flow
during a blocking episode using localized Eliassen-Palm flux diagnostics. J. Atmos. Sci., 43,
2070-2087.
(XYS20091027)
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