Fog climatology at Shanghai Pudong International Airport

IF 2.3 4区 地球科学 Q3 METEOROLOGY & ATMOSPHERIC SCIENCES Meteorological Applications Pub Date : 2024-03-13 DOI:10.1002/met.2191
Ran Hao, Rui Lyu, Xue Hao, Jun Yi, Weijie Wang, Tiantao Cheng, Bo Xu
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Abstract

Using 22-year ground observations on meteorological variables, we conducted a statistical analysis to reveal fog characteristics at Shanghai Pudong International Airport (SPIA). Fog events were classified by fog types using an objective method. Two types of advection fogs are dominant in fog events at SPIA, followed by radiation fogs. Different fogs have evident annual and monthly variations in frequency. Advection fog mostly appear from February to April, while radiation fog is mainly between November and February. Six synoptic patterns associated with fogs were determine by a self-organizing maps cluster method, two of which, namely ‘west of marine high pressure’ and ‘inverted trough’, are most favourable for the formation of advection fogs, whereas ‘bottom of weak cold high-pressure’ is favourable for radiation fogs. The frequency of advection fog occurrence exhibits temporal fluctuations with distinct peaks occurring 2–3 h after sunset, around midnight, and 1–2 h before sunrise, while almost all radiation fog occur in the second half of the night, and favourable conditions for fog onset become more effective with the length of the night. Radiation fog exhibits a longer duration than advection fog and tends to result in lower visibility. The prevalent wind direction for the formation of advection fog is generally from the east to the southeast, whereas radiation fog is typically associated with westerly winds. The temperature and air pressure during the formation of both advection and radiation fogs follow a normal distribution in most seasons. More fog characteristics were categorized by fog types and seasons.

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上海浦东国际机场的雾气候特征
利用 22 年来对气象变量的地面观测数据,我们进行了统计分析,以揭示上海浦东国际机场(SPIA)的雾特征。采用客观方法对雾事件进行了雾类型分类。两种类型的平流雾在上海浦东国际机场的雾事件中占主导地位,其次是辐射雾。不同的雾在频率上有明显的年度和月度变化。平流雾主要出现在二月至四月,而辐射雾主要出现在十一月至次年二月。通过自组织地图聚类方法确定了与雾相关的六种天气模式,其中 "海洋高压以西 "和 "倒槽 "两种模式最有利于平流雾的形成,而 "弱冷高压底部 "则有利于辐射雾的形成。平流雾出现的频率在时间上有波动,日落后 2-3 小时、午夜前后和日出前 1-2 小时出现明显的高峰,而几乎所有辐射雾都出现在后半夜,随着夜长,起雾的有利条件变得更加有效。辐射雾的持续时间比平流雾长,往往导致能见度降低。形成平流雾的主要风向一般是东至东南风,而辐射雾通常与西风有关。平流雾和辐射雾形成时的温度和气压在大多数季节都呈正态分布。更多的雾特征按雾的类型和季节进行了分类。
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来源期刊
Meteorological Applications
Meteorological Applications 地学-气象与大气科学
CiteScore
5.70
自引率
3.70%
发文量
62
审稿时长
>12 weeks
期刊介绍: The aim of Meteorological Applications is to serve the needs of applied meteorologists, forecasters and users of meteorological services by publishing papers on all aspects of meteorological science, including: applications of meteorological, climatological, analytical and forecasting data, and their socio-economic benefits; forecasting, warning and service delivery techniques and methods; weather hazards, their analysis and prediction; performance, verification and value of numerical models and forecasting services; practical applications of ocean and climate models; education and training.
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