2022年春季浙江沿海海面一次持续性海雾过程特征及成因分析
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1.浙江省气象台;2.鄞州区气象局;3.宁波市气象台

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国家自然科学基金项目(42105135),宁波市公益性科技计划重点项目(2022S181),浙江省气象局预报员专项(2021YBY01),浙江省气象局一般项目(2021YB01)


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Characteristics of a persistent sea fog process over Zhejiang coastal waters in spring 2022
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1.Zhejiang Meteorological Observatory,hangzhou;2.Yinzhou Meteorological Observatory,ningbo;3.Ningbo Meteorological Observatory,ningbo

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    摘要:

    2022年4月10—14日浙江沿海海面出现了一次持续时间长、范围广、浓度大的海雾过程。利用卫星资料、ERA Interim再分析资料和浙江沿海自动站观测资料,分析其特征和成因。结果表明,低层逆温层使得低层水汽不易扩散到高空, 有利于大雾的生成和维持。成雾阶段,有明显的水汽辐合,同时气温高于SST且差值在0~2℃。海雾维持且浓度较大时,水汽辐合逐渐减弱;气海温差则基本在0℃左右。消散阶段,有明显的水汽辐散;气海温差大于2℃或小于0℃。

    Abstract:

    From April 10 to 14,2022, a long-duration, wide-range and high-concentration sea fog event occurred in the coastal waters of Zhejiang Province. In this paper, the characteristics and causes are analyzed by using satellite data, ERA Interim reanalysis data and Zhejiang coastal automatic station observation data. The results show that the inversion layer makes it difficult for the low-level water vapor to spread to the upper air, which is conducive to the generation and maintenance of fog. In the fog formation stage, there is obvious water vapor convergence, at the same time, the temperature is higher than SST and the difference is 0-2 °C. In the maintenance stage, water vapor convergence gradually weakened, the air-sea temperature difference is basically around 0 °C. In the dissipation stage, there is obvious water vapor divergence ; the air-sea temperature difference is greater than 2 °C or less than 0 °C.

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  • 收稿日期:2023-01-31
  • 最后修改日期:2023-11-16
  • 录用日期:2024-01-03
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