RESEARCH ARTICLE


A Study of the Effects of the Ice-Microphysics, Surface Friction, and Surface Heat Flux on Tropical Cyclone Formation§



Masanori¶ Yamasaki
16-34 Shirahata kami-cho, Kanagawa-ku, Yokohama, 221-0075, Japan.


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© 2013 Masanori Yamasaki.;

open-access license: This is an open access article distributed under the terms of the Creative Commons Attribution 4.0 International Public License (CC-BY 4.0), a copy of which is available at: https://creativecommons.org/licenses/by/4.0/legalcode. This license permits unrestricted use, distribution, and reproduction in any medium, provided the original author and source are credited.

* Address correspondence to this author at the 16-34 Shirahata kami-cho, Kanagawa-ku, Yokohama, 221-0075, Japan; Tel: 81-45-423-9289; E-mail: mn-yama@lucky.odn.ne.jp
§ Part of this study was made when the author was affiliated with Research Institute for Global Change, Japan Agency for Marine-Earth Science and Technology, Yokohama, Japan, and presented at the 2012 spring meeting of the Meteorological Society of Japan.
MSJ member, AMS emeritus member


Abstract

This paper describes results from numerical experiments which have been performed to understand the effects of the ice microphysics, surface friction, and surface heat flux on tropical cyclone (TC) formation. This study uses the author’s non-hydrostatic model that intends to resolve cumulus convection. However, the horizontal grid size is taken to be somewhat large; 2 km in an area of 600 km x 600 km. A non-uniform coarse grid is used in the surrounding area with 4,000-km square. Several buoyancy perturbations arranged in the west-east direction, and a weak vortex with the maximum wind speed of 5 m s–1 are given at the initial time of the numerical time integrations.

It is confirmed from two numerical experiments with and without ice microphysics that the development of a vortex is slower, and TC formation is delayed, in the presence of ice microphysics. It is also confirmed that a vortex can develop even without surface friction. It is shown that a strong vortex with the maximum wind speed of 20~25 m s–1 can be obtained. As expected, however, no eye forms, and further development does not occur. That is, it is confirmed that surface friction is indispensable to eye formation and a very strong TC having an eye. As for the third concern of this study, it is shown that a vortex with the maximum wind speed of about 5 m s–1 does not develop in the absence of the surface heat flux. That is, the surface heat flux plays an important role even in a weak vortex. Important backgrounds and understandings that are concerned with these results are described, based on studies on TCs in the past 50 years.

Keywords: Cloud Resolving Model, Cumulus-Convection-Resolving Model, Frictional Flow CISK, Ice Microphysics, Nonhydrostatic Model, Surface Friction, Surface Heat Flux, Tropical Cyclone Formation.