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Observational Study on the Characteristics of the Boundary Layer during Changes in the Intensity of Tropical Cyclones Landing in Guangdong, China

机译:中国广东省热带旋风强度变化中边界层特征的观察研究

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Eleven tropical cyclones that landed in Guangdong Province since 2012 and experienced strengthening or weakening over the offshore area were studied. Since the structure of the tropical cyclone boundary layer significantly influences the variation of the intensity of the cyclone, continuous observations of the wind profile radar at a coastal radar station in Guangdong Province were combined with aircraft observation data of the No. 1604 “Nida” cyclone to analyse the variations in the distributions of the radial wind, tangential wind, and angular momentum in the typhoon boundary layer and the similarities and differences between the boundary layers of the 11 tropical cyclones during the strengthening or weakening of their intensities. The analysis results show that the presence of the supergradient wind and the enhancement effect of the radial inflow play important roles in enhancing the intensity of a tropical cyclone. The observations indicate that when the tangential wind velocity in the maximum wind velocity radius reaches the velocity of the supergradient wind and when the radial inflow either gradually increases towards the centre of the tropical cyclone or gradually covers the entire boundary layer, the angular momentum tends to be shifted towards the centre. At this time, the maximum radial inflow, maximum tangential wind, and maximum angular momentum are in the same height range in the vertical direction. When a strong radial outflow occurs in the boundary layer of a tropical cyclone or the area with maximum wind velocity is located in the air outflow, the angular momentum cannot easily be transported towards the centre of the typhoon. Therefore, the spatial configuration of the three physical quantities will determine future changes in the intensity of tropical cyclones. The scope of the results presented here is limited to the 11 selected cases and suggests extending the analysis to more data.
机译:从2012年以来,在广东省降落的11个热带气旋,并在近海地区进行了加强或削弱。由于热带气旋边界层的结构显着影响旋风强度的变化,因此广东省沿海雷达站的风型雷达的连续观察与第1604号“Nida”旋风的飞机观察数据相结合为了分析台风边界层的径向风,切向风和角动量的分布的变化以及11热带气旋在强度的强度期间的边界层之间的相似性和差异。分析结果表明,径向流入的超级风量和增强效果的存在在增强热带气旋的强度方面发挥着重要作用。观察结果表明,当最大风速半径中的切向风速达到超级平衡的速度并且当径向流入朝向热带气旋的中心逐渐增加或逐渐覆盖整个边界层时,角动力趋于转向中心。此时,最大径向流入,最大切向风和最大角动量在垂直方向上处于相同的高度范围。当在热带气旋的边界层或具有最大风速的区域中发生强的径向流出时,在空气流出中,角动量不能容易地朝向台风的中心运输。因此,三种物理量的空间配置将确定热带气旋强度的未来变化。此处呈现的结果的范围仅限于11个选定的情况,并建议将分析扩展到更多数据。

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