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Wang Qian,Shi Xiaomeng,Zhang Suping. Observational Analyses of a Sea Fog Event over the Northern Yellow Sea when Typhoon Lekima (1909) Landed on Qingdao[J]. Haiyang Xuebao,2023, 45(x):1–13
Citation: Wang Qian,Shi Xiaomeng,Zhang Suping. Observational Analyses of a Sea Fog Event over the Northern Yellow Sea when Typhoon Lekima (1909) Landed on Qingdao[J]. Haiyang Xuebao,2023, 45(x):1–13

Observational Analyses of a Sea Fog Event over the Northern Yellow Sea when Typhoon Lekima (1909) Landed on Qingdao

  • Received Date: 2023-01-01
    Available Online: 2023-10-16
  • This study focuses on the physical process of a sea fog event during Typhoon Lekima in the Northern Yellow Sea by using observation data, reanalysis data and backward trajectory model. The analysis indicates that the typhoon circulation was the decisive factor determining whether fog formed offshore and developed inland. The warm and humid southerlies from the south Yellow Sea condensed into fog on the colder sea surface besides the typhoon center, which not only provided sufficient moisture for the formation and development of the sea fog but also formed a significant inversion layer over the fog area with the downdraft in the center of the typhoon. The "stable up and turbulent down" structure in the atmospheric boundary layer improved the development of sea fog on the coast and inland area. However, the horizontal wind steering and the strengthening wind speed behind the typhoon strengthened the wind shear in the atmospheric boundary layer, resulting in the enhanced turbulent mixing and the decrease of the stability in the bottom atmospheric boundary layer, which was the main cause of the fog dissipation.
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