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近年来中卫市大雾天气的分析及预报方法研究

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[目的]提升预报员对低能见度天气"雾"的预报水平.[方法]利用2000-2021年中卫市4个气象站雾日观测资料,对雾的时空分布特征进行分析.结合同期NCEP/NCAR逐日再分析资料,对中卫市雾产生的环流背景和物理特征进行分析,总结出中卫市雾的预报指标.[结果]中卫市雾日分布由北自南减少,年雾日在波动中基本持平.秋季雾出现站次最多,夏季次之,春季雾出现站次最少.中卫市雾天中高层500 hPa上基本为西西北气流,850~700 hPa为偏南气流,地面为均压场.850 hPa相对湿度较大,地面湿度接近饱和,高空风垂直切变也较小.由于高空大气层结稳定,地面水平运动不强,高低空能量交换受到抑制,有利于大雾天气的形成和维持.[结论]根据中卫市雾日要素场特征,得出以下雾的预报指标:①预报次日08时各站地面风速≤4 m/s;②预报次日08时各站云量≤3成;③预报次日08时各站T地面-T850hPa≤0℃;④预报850 hPa次日T-Td≤3℃;⑤预报次日清晨最大相对湿度≥90%;⑥当日14时相对湿度≥60%;⑦预报次日清晨最低气温不超过当日14时的露点温度;⑧预报次日清晨Tmin≤前一天14时的Td.
Analysis and Forecasting Methods of Heavy Fog Weather in Zhongwei City in Recent Years
[Purposes]This paper aims to improve the predictive ability of forecasters for low visibility weather"fog".[Methods]Using fog day observation data from four meteorological stations in Zhongwei City from 2000 to 2021,the spatiotemporal distribution characteristics of fog were analyzed.In addition,combined with daily reanalysis data from NCEP/NCAR during the same period,the circulation back-ground and physical characteristics of fog in Zhongwei City were analyzed,and the forecast indicators for fog in Zhongwei City were summarized.[Findings]The results showed that the distribution of foggy days in Zhongwei City decreased from north to south,and the annual foggy days remained relatively stable in fluctuations;In the foggy days of Zhongwei City,the upper 500 hPa is basically a west-northwest airflow,850~700 hPa is a southerly airflow,and the ground is a uniform pressure field.The relative humidity at 850 hPa is relatively large,the ground humidity is close to saturation,and the vertical wind shear is also relatively small.Due to the stable atmospheric stratification at high altitude,the horizontal movement of the ground is not strong,and the energy exchange between high and low altitude is suppressed,which is conducive to the formation and maintenance of foggy weather.[Conclusions]Based on the characteris-tics of the fog day element field in Zhongwei City,the following forecast indicators for fog are obtained:①ground wind speed at each station at 08:00 the next day is predicted to be≤4 m/s;②it is predicted that the cloud cover at each station will not exceed 30%at 8 am the next day;③it is predicted that at 08:00 the next day,the T ground temperature at each station-T 850 hPa≤0℃;④it is predicted that the next day with 850 hPa T-Td≤3℃;5.Forecast the maximum relative humidity of the next morning to be≥90%;⑥At 14:00 on the same day,the relative humidity≥60%;⑦Forecast that the lowest temperature in the morning of the next day will not exceed the dew point temperature at 2 pm on the same day;⑧it is predicted that the Tmin of the next morning≤the Td at 2 pm of the previous day.

fogspatiotemporal distributioncirculation characteristicsforecasting methods

虎娜、杨苑、陈星宜、杨贵、张泽瑾、尹俊博

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中卫市气象局,宁夏 中卫 755000

衡水市气象局,河北 衡水 053000

时空分布 环流特征 预报方法

2024

河南科技
河南省科学技术信息研究院

河南科技

影响因子:0.615
ISSN:1003-5168
年,卷(期):2024.51(22)