2024年一次青岛近海平流雾的微物理特征观测分析
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1.中国海洋大学深海圈层与地球系统前沿科学中心;2.山东省气象防灾减灾重点实验室;3.中国海洋大学海洋与大气学院;4.青岛市气象台

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P47

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国家自然科学基金联合项目(U2342214);国家自然科学基金面上项目(42475099);长岛国家气候观象台开放基金(2023cdkfz01);风云卫星应用先行计划项目 (FY-APP-ZX-2023.02)


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Observational analysis of the microphysical characteristics of an advection fog event along the coast of Qingdao in 2024
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1.Frontiers Science Center for Deep Ocean Multispheres and Earth System,Ocean University of China;2.Laboratory for Meteorological Disaster Prevention and Mitigation of Shandong;3.College of Oceanic and Atmospheric Sciences,Ocean University of China;4.Qingdao Meteorological Bureau

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    摘要:

    2024年5月22日至25日青岛近海发生了一次平流雾过程,我们同时在八关山和小麦岛两个沿海站点使用FM-120型雾滴谱仪开展了海雾微物理特征观测,并结合地面自动站观测资料和ERA5(ECMWF Reanalysis v5,ERA5)再分析数据,分析了本次海雾过程。结果表明:此次海雾过程具有稳定的天气形势、东南暖湿气流以及较强的逆温结构。整个海雾过程中,八关山平均数浓度为277.02 cm?3,平均含水量为0.051 g m?3,平均有效半径为4.92 μm,平均半径为2.65 μm;小麦岛平均数浓度为77.58 cm?3,平均含水量为0.027 g m?3,平均有效半径为7.39 μm,平均半径为2.78 μm。两个观测点的微物理特征随时间同步演变,雾滴谱分布在海雾的发展成熟阶段具有明显双峰结构,尤其在在15 μm以上的大粒径段上抬明显。本次海雾过程中,基于数浓度和含水量共同建立的能见度参数化方案,预测效果最佳。

    Abstract:

    From May 22 to 25, 2024, an advection fog event occurred along the coast of Qingdao. This study analyzes the microphysical characteristics of the sea fog at two coastal observation sites, Baguan Hill and Xiaomai Island, using data from an FM-120 fog monitor, surface automatic station observations, and ERA5 (ECMWF Reanalysis v5) reanalysis data. The results indicated that the fog event was characterized by stable weather conditions, southeast warm moist airflow, and a strong inversion layer. During the event, the average number concentration at Baguan Hill is 277.02 cm?3, with an average liquid water content of 0.051 g m?3, an average effective radius of 4.92 μm, and an average radius of 2.65 μm. At Xiaomai Island, the average number concentration is 77.58 cm?3, with an average liquid water content of 0.027 g m?3, an average effective radius of 7.39 μm, and an average radius of 2.78 μm. The microphysical characteristics from both observation points exhibited synchronous temporal evolution, and the droplet size distribution displayed a distinct bimodal structure during the development and maturation of the fog, particularly evident in the large particle range above 15 μm. The visibility parameterization scheme established based on both number concentration and liquid water content shows optimal predictive performance during the fog event.

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  • 收稿日期:2025-01-24
  • 最后修改日期:2025-04-04
  • 录用日期:2025-04-11
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