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

Journal of Meteorology and Environment ›› 2020, Vol. 36 ›› Issue (3): 87-92.doi: 10.3969/j.issn.1673-503X.2020.03.012

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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

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

CLC Number: