## Abstract The linear model for the steady boundary layer of a rapidly rotating axisymmetric vortex is derived from a detailed scale analysis of the full equations of motion. The previously known analytic solution is reβappraised for vortices of hurricane scale and strength. The internal consisten
Erratum: Limitations of a linear model for the hurricane boundary layer. Stefanie Vogl and Roger K. Smith
- Publisher
- John Wiley and Sons
- Year
- 2009
- Tongue
- English
- Weight
- 28 KB
- Volume
- 135
- Category
- Article
- ISSN
- 0035-9009
- DOI
- 10.1002/qj.470
No coin nor oath required. For personal study only.
β¦ Synopsis
Abstract
The above article originally published on Early View 15 April 2009 and subsequently in issue 135(641): 839β850. DOI: 10.1002/qj.390
It has since been noted that on pages 839, 840, 845, 846, 847, 848 and 849 there were citations to βKepert (2001)β, however, this citation was not included in the reference list.
The following is the missing reference which should be included within the article's reference list:
Kepert, JD. 2001. The dynamics of boundary layer jets within the tropical cyclone core. Part I: Linear theory. J. Atmos. Sci. 58: 2469β2484.
π SIMILAR VOLUMES
## Abstract A simple slab model for the boundary layer of a hurricane is reβexamined and a small error in the original calculation is corrected. With this correction, the development of supergradient winds is a ubiquitous feature of the solutions. The boundary layer shows two types of behaviour in
## Abstract We present a critique of Emanuel's steadyβstate hurricane model, which is a precursor to his theory for hurricane potential intensity (PI). We show that a major deficiency of the theory is the tacit assumption of gradient wind balance in the boundary layer, a layer that owes its existen