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In order to understand the effects of cumulus convection on large-scale atmospheric motions, heat and moisture budget analyses are often performed using data from an array of radiosonde stations. Ever since the pioneering work of Yanai et al. (1973),
Externí odkaz:
http://arxiv.org/abs/1810.11119
Autor:
Schubert, Wayne H.
This paper is the textual material accompanying the 2017 Bernhard Haurwitz Memorial Lecture, delivered by the author on 28 June 2017, at a joint session of the American Meteorological Society's 21st Conference on Atmospheric and Oceanic Fluid Dynamic
Externí odkaz:
http://arxiv.org/abs/1801.08238
This paper discusses some basic concepts that arise in the study of the tropical cyclone frictional boundary layer. Part I discusses the concepts of asymptotic triangular waves and asymptotic N-waves in the context of the nonlinear advection equation
Externí odkaz:
http://arxiv.org/abs/1709.00101
When studying tropical cyclones using the $f$-plane, axisymmetric, gradient balanced model, there arises a second-order elliptic equation for the transverse circulation. Similarly, when studying zonally symmetric meridional circulations near the equa
Externí odkaz:
http://arxiv.org/abs/1705.05460
This paper presents numerical solutions and idealized analytical solutions of axisymmetric, $f$-plane models of the tropical cyclone boundary layer. In the numerical model, the boundary layer radial and tangential flow is forced by a specified pressu
Externí odkaz:
http://arxiv.org/abs/1405.7939
Publikováno v:
Journal of Climate, 2018 Jun 01. 31(11), 4543-4562.
Externí odkaz:
https://www.jstor.org/stable/26496167
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Akademický článek
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Autor:
Schubert, Wayne H., Taft, Richard K.
Publikováno v:
Frontiers in Earth Science. 10
The problem of tropical cyclone rapid intensification is reduced to a potential vorticity (PV) equation and a second order, inhomogeneous, partial differential equation for the azimuthal wind. The latter equation has the form of a Klein-Gordon equati
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::bc6fd1aa3ffbcbb3cec1c0ecf79dec0d
https://doi.org/10.3389/feart.2022.1038351
https://doi.org/10.3389/feart.2022.1038351
Publikováno v:
Meteorology; Jun2023, Vol. 2 Issue 2, p191-221, 31p