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首页> 外文期刊>Mathematical Problems in Engineering: Theory, Methods and Applications >Comparative Study of the Near-Surface Typhoon Wind Profile Fitting between Offshore and Onshore Areas
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Comparative Study of the Near-Surface Typhoon Wind Profile Fitting between Offshore and Onshore Areas

机译：Comparative Study of the Near-Surface Typhoon Wind Profile Fitting between Offshore and Onshore Areas

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摘要

The study of typhoon wind profiles, especially offshore typhoon wind profiles, has been constrained by the scarcity of observational data. In this study, the Doppler wind lidar was used to observe the offshore wind profiles during Super Typhoon Mangkhut and onshore wind profiles during Super Typhoon Lekima. Four wind profile models, including the power law, logarithmic law, Deaves-Harris (D-H), and Gryning, were selected in the height range of 0-300 m to fit the wind profile. The variations in the power exponent with the mean wind speed and roughness length were also analyzed. The results showed that the wind profiles fitted by the four models were generally in good agreement with the observed wind profiles with correlation coefficients greater than 0.98 and root mean square deviations less than 0.5 m s(-1). For the offshore case, the fitting degree of all wind profile models improved with increasing mean wind speed. Specifically, the D-H model had the highest fitting degree when the horizontal mean wind speed at 40 m was in the range of 8-25 m s(-1), while the log-law model had the highest fitting degree when the wind speed exceeded 30 m s(-1). For the onshore case, the fitting degree of the four wind profile models deteriorated with increasing mean wind speed, and the log-law model had the highest fitting degree in all wind speed intervals from 8 to 30 m s(-1). For both offshore and onshore cases, the power exponent was less affected by mean wind speed and increased with increasing roughness length, and the logarithmic empirical model proposed in this study could well characterize the relationship between the power exponent and roughness length.

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