The Role of Boundary Layer Dynamics in Tropical Cyclone Intensification. Part I: Sensitivity to Surface Drag Coefficient-Reference-Cited by-同舟云学术

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The Role of Boundary Layer Dynamics in Tropical Cyclone Intensification. Part I: Sensitivity to Surface Drag Coefficient

Published:2021 Issue:2 Volume:99 Page:537-554
ISSN:0026-1165
Container-title:Journal of the Meteorological Society of Japan. Ser. II
language:en
Short-container-title:Journal of the Meteorological Society of Japan

Author:

LI Tsung-Han¹,WANG Yuqing²^ORCID

Affiliation:

1. Department of Atmospheric Sciences and International Pacific Research Center, University of Hawai'i, Hawai'i, USA

2. State Key Laboratory of Severe Weather (LaSW), Chinese Academy of Meteorological Sciences, China Meteorological Administration, China

Publisher

Meteorological Society of Japan

Subject

Atmospheric Science

Link

https://www.jstage.jst.go.jp/article/jmsj/99/2/99_2021-027/_pdf

Reference61 articles.

1. Charney, J. G., and A. Eliassen, 1964: On the growth of the hurricane depression. J. Atmos. Sci., 21, 68-75.

2. Craig, G. C., and S. L. Gray, 1996: CISK or WISHE as the mechanism for tropical cyclone intensification. J. Atmos. Sci., 53, 3528-3540.

3. DeMaria, M., and W. H. Schubert, 1984: Experiments with a spectral tropical cyclone model. J. Atmos. Sci., 41, 901-924.

4. Donelan, M. A., 2018: On the decrease of the oceanic drag coefficient in high winds. J. Geophys. Res.: Oceans, 123, 1485-1501.

5. Durran, D. R., and J. B. Klemp, 1983: A compressible model for the simulation of moist mountain waves. Mon. Wea. Rev., 111, 2341-2361.

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