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2004•Journal of Tropical MeteorologyRequires access

CONSTRUCTION OF WIND SPEED IN TYPHOON ON OCEAN SURFACE

Xiaogang Huang

Open publisher page 1 citations

Abstract

In this paper, we first adopt the asymmetric maximum wind velocity and radius of the maximum wind velocity formulas, and then use the optimal coefficient scheme to get the parameter which controls the distribution of the typhoon wind outer structure with the consideration of real 30 knots and 50 knots wind radius. In addition, we improve the tangential wind profile scheme of typhoon brought forward by Chan and Williams (1987) and then typhoon ocean surface asymmetric wind speed is shown. The experiment shows that this method can describe the asymmetry distribution of wind speed in typhoon over the ocean surface and would have a broad prospect for operational practice.

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What this paper is about

In this paper, we first adopt the asymmetric maximum wind velocity and radius of the maximum wind velocity formulas, and then use the optimal coefficient scheme to get the parameter which controls the distribution of the typhoon wind outer structure with the consideration of real 30 knots and 50 knots wind radius. In addition, we improve the tangential wind profile scheme of typhoon brought forward by Chan and Williams (1987) and then typhoon ocean surface asymmetric wind speed is shown. The experiment shows that this method can describe the asymmetry distribution of wind speed in typhoon over the ocean surface and would have a broad prospect for operational practice.

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Available abstract

In this paper, we first adopt the asymmetric maximum wind velocity and radius of the maximum wind velocity formulas, and then use the optimal coefficient scheme to get the parameter which controls the distribution of the typhoon wind outer structure with the consideration of real 30 knots and 50 knots wind radius. In addition, we improve the tangential wind profile scheme of typhoon brought forward by Chan and Williams (1987) and then typhoon ocean surface asymmetric wind speed is shown. The experiment shows that this method can describe the asymmetry distribution of wind speed in typhoon over the ocean surface and would have a broad prospect for operational practice.

Key concepts: Typhoon, Wind speed, Wind profile power law, Meteorology, Maximum sustained wind, RADIUS, Environmental science, Asymmetry

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