琼州海峡大雾天气形势特征分析
作者:
作者单位:

1.徐闻县气象局,广东 徐闻 524100 ;2.翁源县气象局,广东 翁源 512600 ;3.广东海洋大学,广东 湛江 524088 ;4.广东省近海海洋变化与灾害预警实验室,广东 湛江 524088 ;5.湛江市气象局,广东 湛江 524001

作者简介:

张新新,327306710@qq.com。
吴德平,zjwdp@126.com。

通讯作者:

中图分类号:

P426.4;P47

基金项目:

湛江市气象局科学技术研究项目(2021A02);广东省气象局科学技术研究项目(GRMC2024M29);广东省科技计划项目(2024B1212040002);广东省教育厅创新团队项目(2023KCXTD015)


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Analysis on characteristics of synoptic situations of dense fog in the Qiongzhou Strait
Author:
Affiliation:

1.Xuwen Meteorological Service, Xuwen 524100 , China ; 2.Wengyuan Meteorological Service, Wengyuan 512600 , China ; 3.Guangdong Ocean University, Zhanjiang 524088 , China ; 4.Guangdong Key Laboratory for Coastal Ocean Variation and Disaster Prediction, Zhanjiang 524088 , China ; 5.Zhanjiang Meteorological Service, Zhanjiang 524001 , China

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    摘要:

    利用1990—2023年徐闻国家级气象观测站地面观测资料和NCEP/NCAR再分析资料,对琼州海峡发生大雾的气候变化特征、气象要素特征以及成雾的常见天气形势进行统计分析。结果表明:(1)琼州海峡年均大雾日数为16.6 d,雾日数年际变化总体呈减少趋势。冬季琼州海峡大雾出现频率最高,占全年的51.8%,夏季最少,占7.8%。2月琼州海峡大雾日数最多,平均大雾日数为4.2 d,占全年的25.3%;7月的平均大雾日数最少,仅为0.3 d。琼州海峡大雾主要出现在04—08时,占全天的42.7%,峰值出现在06时,谷值在13时。(2)琼州海峡出现大雾的理想气象条件为,地面盛行偏东风(东东北—东东南风),风速集中在[1.0,5.0) m·s-1;气温处于[16,22) ℃;温度露点差t-td≤2.0 ℃;本站气压为[1 005.0,1 017.5] hPa;相对湿度大于90%。(3)琼州海峡出现大雾的环流形势可分为低压前型、高压入海型、静止锋型、冷锋前型和均压场型5类,各个分型占所有大雾天气过程的比例分别为10.8%、13.5%、21.6%、24.3%、29.8%,其中低压前型和高压入海型主要产生平流雾,静止锋型多出现混合雾,冷锋前型产生锋面雾,均压场型主要产生辐射雾;所分5种天气形势类型及其产生的大雾类型可为实际业务提供参考价值。

    Abstract:

    Using the ground observation data of Xuwen National Meteorological Observing Station from 1990 to 2023 and the NCEP/NCAR reanalysis data, the characteristics of climate change, meteorological elements and common synoptic situations of the occurrence of dense fog in the Qiongzhou Strait are statistically analyzed. The results are shown below. (1) The annual average number of foggy days in the Qiongzhou Strait is 16.6 d, and the interannual change of foggy days presents a decreasing trend. Winter is the season with the highest frequency of dense fog in the Qiongzhou Strait, accounting for 51.8% of the annual total number of dense fog days, while summer sees the lowest frequency, making up only 7.8%. February is the month with the most dense fog days in the Qiongzhou Strait with an average of 4.2 d, accounting for 25.3% of the annual total number of dense fog days, while July has the least average number of dense fog days (only 0.3 d). The dense fog in the Qiongzhou Strait mainly occurs from 04:00 to 08:00, accounting for 42.7% of the whole day; the peak appears at 06:00, and the valley at 13:00. (2) The ideal meteorological conditions for the formation of dense fog in the Qiongzhou Strait are as follows: the easterly wind (ENE-ESE) prevails on the surface with the wind speed concentrated in the range of [1.0,5.0) m·s-1, the temperature is in the range of [16,22) ℃, the depression of the dew point (t-td) does not exceed 2.0 ℃, the pressure is in the range of [1 005.0,1 017.5] hPa at the station, and the relative humidity is higher than 90%. (3) The circulation patterns of the fog in the Qiongzhou Strait can be divided into 5 types: the front low pressure, the high pressure entering the sea, the stationary front, the front of cold front and the equal pressure field, which account for 10.8%, 13.5%, 21.6%, 24.3% and 29.8%, respectively. Among them, the front low pressure type and the high pressure entering the sea type mainly produce advection fog, the stationary front type often produces mixing fog, the front of cold front type produces frontal fog and the equal pressure field type mainly produces radiation fog. The 5 types of weather patterns and the fog types they generate provide reference for practical operations.

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张新新,赵亮巨,龙景超,等.琼州海峡大雾天气形势特征分析[J].海洋气象学报,2025,45(3):42-50.

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  • 收稿日期:2025-02-28
  • 最后修改日期:2025-04-24
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  • 在线发布日期: 2025-07-01
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