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台风背景下基于北部湾海岛多层观测的风场及空气动力学参数特征分析

Study on the characteristics of wind field and aerodynamic parameters based on multi-level observations on the Beibu Gulf island under typhoon conditions

  • 摘要: 基于广西北海涠洲岛近地面层多层观测数据,选取2023–2024年台风摩羯、三巴和泰利影响时段,首先对各台风过程的观测数据进行质量控制和订正,随后分析北部湾海岛复杂下垫面影响下的台风边界层结构特征,主要包括近地面层风场演变,风廓线特征及空气动力学参数(摩擦速度u*、粗糙度长度z0和拖曳系数Cd)随近地面风速和风向的变化特征。研究表明,10–32 m的台风边界层接近中性稳定层结,平均风速廓线符合对数律分布。在北部湾海岛复杂下垫面作用下,u*、z0和Cd随近地面风速的变化特征接近陆地下垫面影响情况,均表现出明显的非单调性,不能简单归为均质海洋下垫面情况。其中,u*的数值范围为0.5–1.5 m s-1;当10 m风速高于15 m s-1附近时,z0和Cd的量级分别为10-2 m和10-3;偏东风影响下的u*、z0和Cd数值较偏西风条件下偏大。研究结果有利于加深对复杂海岛下垫面类型下台风边界层结构的理解与认识,对北部湾区域台风数值模拟及参数化方案的优化具有重要意义。

     

    Abstract: Based on multi-level observation data from near-surface layer on the Weizhou Island, Beihai, Guangxi, the study selected the periods influenced by Typhoons Yagi, Sanba, and Talim during 2023–2024. First, quality control and correction were performed on the observation data for each typhoon event. Subsequently, the structural characteristics of typhoon boundary layer under the influence of complex underlying surface on the Beibu Gulf island were analyzed. This included the evolution of near-surface wind fields, wind profile characteristics, and the variations of aerodynamic parameters, i.e., friction velocity (u*), roughness length (z0), and drag coefficient (Cd), with near-surface wind speed and direction. The results indicate that the typhoon boundary layer between 10–32 m exhibits near-neutral stability, and the mean wind speed profile follows logarithmic distribution. Under the influence of complex underlying surface on the Beibu Gulf island, the variations of u*, z0, and Cd with near-surface wind speed resemble characteristics typical of land underlying surface, showing obvious non-monotonicity and cannot be simply categorized as homogeneous marine underlying surface condition. Specifically, u* ranges between 0.5–1.5 m s-1; when the 10 m wind speed exceeds approximately 15 m s-1, the magnitudes of z0 and Cd are on the order of 10-2 m and 10-3, respectively. Under easterly winds, the values of u*, z0, and Cd are generally higher than those under westerly winds. The findings contribute to deeper understanding of typhoon boundary layer structure over complex island underlying surface and hold significant importance for optimizing typhoon numerical simulations and parameterization schemes in the Beibu Gulf region.

     

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