基于逐時資料的黃山霧凇特征及氣象條件分析
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安徽省氣象局科技發展基金項目(KM201603)“山岳型景區氣象景觀預報技術研究”資助


Climatic Features and Meteorological Conditions of Rime in Huangshan Based on Hourly Data
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    摘要:

    利用2004—2016年黃山氣象站逐日、逐時地面氣象觀測資料分析了霧凇的時間分布特征及氣象條件。結果表明:①黃山年平均霧凇日616 d,年份之間差異明顯;霧凇初日主要在11月,終日主要在3—4月;連續霧凇日數多在3~4 d,占40%,各年均出現了連續霧凇日數≥10 d的情況。②霧凇出現在10月至次年4月,其中12月至次年3月霧凇日數占898%;月平均霧凇日數與月平均氣溫呈顯著負相關。霧凇還存在一定的日變化,08:00—09:00最多,18:00最少。③逐日資料統計表明,適宜霧凇出現的氣象條件是霧日且日平均氣溫在-8~2 ℃之間、平均相對濕度≥80%、平均風速2~9 m/s。④逐時資料統計表明,霧凇的形成主要受氣溫影響,霧凇形成前需7 h以上的累計低溫(≤0 ℃),適宜霧凇形成的氣象條件是有霧且氣溫在-6~1 ℃之間,濕度≥95%,風速2~11 m/s,較好地反映了霧凇形成的臨界氣象條件。

    Abstract:

    Based on the daily and hourly surface meteorological observation data of Huangshan Station from 2004 to 2016, the temporal distribution and climatic conditions of rime are analyzed. The results show that: (1) The annual average number of rime days in Huangshan is 616, with obvious differences between years. The earliest day of rime was mainly in November and the latest day was mainly in March and April. The number of consecutive rime days is often 3 to 4 days, accounting for 40% of the total number. In each year there were continuous rime days of ≥ 10 days. (2) The rime appeared mainly from October to next April, of which the number of rime days from December to next March accounted for 898%. The monthly mean number of rime days is significantly negatively correlated with the monthly mean temperature. There was a certain daily change in rime, with the highest number at 09:00, and the least at 18:00 (3) Analysis results of daily data show that suitable meteorological conditions for rime are: foggy days and daily mean temperature between -8 and 2 ℃, daily mean humidity ≥ 80%, daily mean wind speed between 2 and 9 m/s. (4) The statistics of hourly data shows that rime formation is mainly affected by air temperature. There needs a period of ≤ 0 ℃ low temperature of more than 7 hours before the formation of rime. The suitable meteorological conditions for rime are foggy and the temperature being between -6 and 1 ℃, humidity ≥ 95%, wind speed between 2 and 11 m/s, which reflect well the critical conditions of rime formation.

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丁國香,劉安平,楊彬,姚葉青.基于逐時資料的黃山霧凇特征及氣象條件分析[J].氣象科技,2018,46(6):1287~1290

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  • 收稿日期:2018-01-04
  • 定稿日期:2018-04-03
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  • 在線發布日期: 2018-12-27
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