山东区域性辐射雾时空分布及地面气象要素特征分析
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郭俊建,男,硕士,高级工程师,主要从事天气预报及业务系统研发,50665523@qq.com。

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中国气象局预报员专项(CMAYBY2017-040);国家自然科学基金项目(41475038)


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Analysis of spatio-temporal distribution of regional radiation fog and characteristics of key meteorological elements in Shandong
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    摘要:

    选取2016—2019年共61次山东区域性辐射雾天气过程,利用山东122个国家级气象观测站逐小时观测资料,对其时空分布及地面气象要素特征进行分析。结果表明:1)山东辐射雾具有显著的季节和日变化特征,主要发生在10月—次年2月,持续性大雾主要发生在1月和12月,一天中20时以后大雾频次增加,02—08时为雾最集中的时段,07时前后达到峰值,下午一般无强浓雾出现。2)辐射雾空间分布呈现明显“西多东少”格局,主要出现在鲁西北和鲁西南地区,山区和半岛沿海地区较少,强浓雾和特强浓雾主要分布在德州、聊城及菏泽等地。3)区域性辐射雾发生时,地面无突出风向,北风略占优势,风速多在3 m·s-1以下;各等级雾形成前气温和露点温度均存在不同程度的下降,20时气温与次日最低气温温差在2~6 ℃、14时地面露点与最低能见度时刻地面露点的温差在1~5 ℃时最有利于辐射雾的发生;随着辐射雾强度的增强,对温度露点差和地面相对湿度的要求越来越高,出现大雾时的温度露点差主要在2 ℃以下,相对湿度大于90%;出现浓雾、强浓雾和特强浓雾时的温度露点差小于1 ℃,相对湿度大于95%。

    Abstract:

    Based on the hourly observation data from 122 national meteorological stations in Shandong, the spatio-temporal distribution of 61 regional radiation fog processes in Shandong from 2016 to 2019 and characteristics of key meteorological elements are analyzed. The results are shown below. 1) There is an evident seasonal variation for radiation fog, which occurs most frequently from October to next February, and long-lasting heavy fog occurs most frequently in January and December. Its diurnal variation is also significant, the fog frequency increases from 20:00 to 07:00 next day with the high frequency during the period from 02:00 to 08:00 and the peak at around 07:00, while there is usually no thick radiation fog in the afternoon. 2) The radiation fog occurs more frequently in the west than in the east of Shandong. In detail, more fog events occur over the northwest and southwest of Shandong and less in the mountainous areas and coastal regions. The thick fog and dense fog events with the visibility lower than 200 m are mainly distributed in Dezhou, Liaochen, and Heze. 3) When the regional radiation fog occurs, the meteorological elements have the following characteristics. There are no significantly preferred wind directions although the northerly overwhelms the others to some degree, and the wind speed is mostly less than 3 m·s-1. The air temperature and dew point both decreases before the formation of all levels of fogs, and radiation fog tends to occur when the difference between the air temperature at 20:00 and the minimum air temperature of the following day lies between 2 ℃ and 6 ℃ and the difference between the dew point at 14:00 and that of the instant the minimum visibility occurs lies between 1 ℃ and 5 ℃. The heavier the fog, the higher the requirements for lower depression of the dew point and higher relative humidity. Most of the fog events with the visibility lower than 1 000 m are accompanied with the depression of the dew point lower than 2 ℃ and relative humidity higher than 90%. When the fog events with the visibility lower than 500 m occur, the depression of the dew point decreases to be lower than 1 ℃ and the relative humidity increases to be more than 95%.

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郭俊建, 韩永清,赵勇.山东区域性辐射雾时空分布及地面气象要素特征分析[J].海洋气象学报,2020,40(2):96-102.

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  • 收稿日期:2020-05-11
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  • 在线发布日期: 2020-07-17
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