主办单位:中国气象局沈阳大气环境研究所
国际刊号:ISSN 1673-503X
国内刊号:CN 21-1531/P

气象与环境学报 ›› 2020, Vol. 36 ›› Issue (3): 87-92.doi: 10.3969/j.issn.1673-503X.2020.03.012

• 论文 • 上一篇    下一篇

1999—2018年锦州地区大雾气候特征及成因分析

张翠艳1(),阎琦2,*(),白雪1,张广梅3,娄芳蕾1,周福然1,常姝婷1   

  1. 1. 锦州市气象局, 辽宁 锦州 121000
    2. 辽宁省气象台, 辽宁 沈阳 110166
    3. 辽宁省气象服务中心, 辽宁 沈阳 110166
  • 收稿日期:2019-05-28 出版日期:2020-06-30 发布日期:2020-07-09
  • 通讯作者: 阎琦 E-mail:zhangcuiyan2008@163.com;yq.mete@163.com
  • 作者简介:张翠艳,女, 1974年生,高级工程师,主要从事天气预报研究, E-mail:zhangcuiyan2008@163.com
  • 基金资助:
    国家重点研发计划项目(2018YFC1507305);中国气象局预报员专项(CMAYBY2019-024);辽宁省气象局重点科研项目(201802)

Climate characteristics and causes of heavy fog in Jinzhou from 1999 to 2018

Cui-yan ZHANG1(),Qi YAN2,*(),Xue BAI1,Guang-mei ZHANG3,Fang-lei LOU1,Fu-ran ZHOU1,Shu-ting CHANG1   

  1. 1. Jinzhou Meteorological Service, Jinzhou 121000, China
    2. Liaoning Meteorological Observatory, Shenyang 110166, China
    3. Liaoning Meteorological Service Center, Shenyang 110166, China
  • Received:2019-05-28 Online:2020-06-30 Published:2020-07-09
  • Contact: Qi YAN E-mail:zhangcuiyan2008@163.com;yq.mete@163.com

摘要:

应用常规气象观测资料、能见度仪观测资料,分析1999—2018年锦州地区大雾气候特征及成因。结果表明:锦州地区雾日年总频次多年平均为33次,存在12 a、6 a和3 a的变化周期。锦州地区典型大雾过程主要分为弱低压槽型、雨后弱高压型。大雾存在日变化。雾前T-Td为4—14℃,风速为4 m·s-1以下,偏南风占50%,偏北风占38%,静风占12%;雾发展阶段T-Td为0—4℃,平均风速为2.2 m·s-1,偏南风占58%,偏北风占42%;浓雾阶段T-Td为0—2℃,平均风速为1.9 m·s-1,偏南风占58%,偏北风占42%;雾减弱到消散阶段T-Td逐渐升高,平均风速为3.3 m·s-1,偏北风占58%。大雾期间,均出现逆温和湿层。

关键词: 大雾, 周期性, 突变性, 合成分析, 水平物理量, 垂直物理量

Abstract:

Based on the conventional meteorological data and visibility observed by visibility meter, the climate characteristics and causes of heavy fog in Jinzhou area during 1999-2018 were investigated.The results show that the annual number of fog days in Jinzhou has 12-year, 6-year and 3-year cycles, and its climatological normal is 33 days.The typical fog process in Jinzhou area shows an obvious diurnal variation, and is mainly divided into weak low pressure trough type and weak high pressure type after rain according to weather classification.Before the fog occurs, T-Td is between 4-14 ℃, the wind speed is generally below 4 m·s-1, the southerly, the northerly and the static wind account for 50%, 38%, and 12%, respectively.During the fog development phase, T-Td is between 0 and 4 ℃, the average wind speed is 2.2 m·s-1, the southerly and the northerly winds account for 58% and 42%, respectively.During the dense fog phase, T-Td is between 0 and 2 ℃, the average wind speed is 1.9m/s, the southerly and the northerly winds account for 58% and 42%, respectively.However, during the fog weakening to the dissipating phase, T-Td is gradually rising and is over 8.1 ℃, the average wind speed is 3.3 m·s-1, and the northerly wind accounts for 58%.As the dense fog appears, temperature inversion and wet layer occur in the atmosphere.

Key words: Heavy fog, Periodicity, Abruptness, Synthetic analysis, Horizontal physical quantity, Vertical physical quantity

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