期刊名称：Journal of Advances in Modeling Earth Systems
电子版ISSN：1942-2466
出版年度：2010
卷号：2
期号：3
页码：1-13
DOI：10.3894/JAMES.2010.2.7
出版社：John Wiley & Sons, Ltd.
摘要：This paper examines the usefulness of the complementary concepts of Rossby length and Rossby depth. These concepts are discussed in the context of idealized analytical solutions of the transverse circulation equation that arises in the balanced vortex model of tropical cyclones. When its coefficients can be considered as constants, this elliptic partial differential equation for the transverse circulation is solved in three different ways: (i) First perform a vertical transform to obtain a radial structure equation, from which arises the concept of a spectrum of Rossby lengths; (ii) First perform a radial transform to obtain a vertical structure equation, from which arises the concept of a spectrum of Rossby depths; (iii) First solve the elliptic PDE directly, without regard to boundary conditions, and then enforce the boundary conditions using the method of image circulations. For weak vortices, Rossby lengths are large and Rossby depths are small, so that the secondary circulation is horizontally elongated and vertically compressed. For strong vortices, Rossby lengths are small and Rossby depths are large, so that the secondary circulation is more vertically elongated and so horizontally compressed that some of the eyewall updraft can return as subsidence in the eye. For strong vortices, the secondary circulation associated with eyewall diabatic heating can be significantly suppressed by the large inertial stability in the interior of the vortex. The large variations of Rossby depth with vortex strength also have important implications concerning how far Ekman pumping can penetrate vertically; only strong vortices have large enough Rossby depths to allow Ekman pumping to penetrate deep into the troposphere.
