霧>浮塵>霾>煙幕>揚(yáng)沙>沙塵暴>吹雪>雪暴。②輕霧和霧年發(fā)生日數(shù)為分別為176 d/a和29 d/a,日發(fā)生概率分別為48%和8%,遠(yuǎn)高出其他天氣現(xiàn)象。③季節(jié)變化方面,霧和輕霧主要出現(xiàn)在秋季和冬季;霾、吹雪和雪暴集中出現(xiàn)在冬季;浮塵發(fā)生春季;揚(yáng)沙多發(fā)生在冬季和春季;而沙塵暴、煙幕主要發(fā)生在春季和秋季。④變化趨勢(shì)上輕霧基本保持平穩(wěn);煙幕呈增加趨勢(shì);而霧、霾、沙塵暴、揚(yáng)沙和浮塵呈下降趨勢(shì)。⑤大氣層結(jié)穩(wěn)定、水汽充足、風(fēng)速較小、人口集中和排放量較大,易于盆地霧、輕霧、霾和煙幕的形成;不合理利用水和土地資源,北方地區(qū)沙塵天氣隨冷空氣南下,是沙塵天氣發(fā)生的重要原因;而吹雪和雪暴均發(fā)生在冬季降雪量大且風(fēng)速較大的川西高原。"/>
1981—2013年四川省視程障礙類天氣現(xiàn)象分析
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國(guó)家自然科學(xué)基金“青藏高原熱力強(qiáng)迫與印度洋的相互作用及其對(duì)亞洲夏季風(fēng)的影響”(41605038)、四川省氣象局課題“氣象臺(tái)站歷史沿革數(shù)據(jù)質(zhì)量控制與可視化系統(tǒng)”(2015開(kāi)發(fā)18)資助


Distribution Characteristics of LowVisibility Weather Phenomena in Sichuan Province from 1981 to 2013
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    利用四川省1981—2013年霧、輕霧、吹雪、雪暴、煙幕、霾、沙塵暴、揚(yáng)沙和浮塵9種視程障礙天氣現(xiàn)象資料,對(duì)其發(fā)生日數(shù)、發(fā)生概率和分布特征進(jìn)行統(tǒng)計(jì)。結(jié)果表明:①各天氣現(xiàn)象發(fā)生日數(shù)排序?yàn)椋狠p霧>霧>浮塵>霾>煙幕>揚(yáng)沙>沙塵暴>吹雪>雪暴。②輕霧和霧年發(fā)生日數(shù)為分別為176 d/a和29 d/a,日發(fā)生概率分別為48%和8%,遠(yuǎn)高出其他天氣現(xiàn)象。③季節(jié)變化方面,霧和輕霧主要出現(xiàn)在秋季和冬季;霾、吹雪和雪暴集中出現(xiàn)在冬季;浮塵發(fā)生春季;揚(yáng)沙多發(fā)生在冬季和春季;而沙塵暴、煙幕主要發(fā)生在春季和秋季。④變化趨勢(shì)上輕霧基本保持平穩(wěn);煙幕呈增加趨勢(shì);而霧、霾、沙塵暴、揚(yáng)沙和浮塵呈下降趨勢(shì)。⑤大氣層結(jié)穩(wěn)定、水汽充足、風(fēng)速較小、人口集中和排放量較大,易于盆地霧、輕霧、霾和煙幕的形成;不合理利用水和土地資源,北方地區(qū)沙塵天氣隨冷空氣南下,是沙塵天氣發(fā)生的重要原因;而吹雪和雪暴均發(fā)生在冬季降雪量大且風(fēng)速較大的川西高原。

    Abstract:

    Based on the observation data of nine kinds of lowvisibility phenomena (mist, fog, snowstorm, blowing snow, smoke, haze, sand storm, blowing sand, and dust) in Sichuan Province from 1981 to 2013, we discuss the number of occurrence days, occurrence probability, and space distribution characteristics. The results show that the number of occurrence days of lowvisibility phenomena in Sichuan Province was: mist > fog > haze > dust > smoke > blowing sand > sandstorm > blowing snow > snowstorm. The numbers of mist and fog days were 176 days and 29 days, and the probability of daily occurrence was 48% and 8%, far higher than other weather phenomena. As for seasonal variation, fog and haze mainly occurred in autumn and winter, and haze, blowing snow, and snowstorm in winter, sand dust in spring, dust storms mainly in winter and spring, and smoke mainly in spring and autumn. The trend of mist in Sichuan remained stable; the smoke was increasing; and the fog, haze, sandstorm, blowing sand and dust were descending. The stable atmosphere, sufficient water vapor, week wind, concentrated population and large emissions were favorable to the formation of fog, mist, basin haze and smoke. Unreasonable use of water and land resources and dust weather in North China along with the southward movement of cold air are the important causes of sand dust weather. Blowing snow and snowstorm occurred in the western Sichuan plateau with larger winter snowfall and higher wind speed.

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黃曉龍,王麗偉,吳薇,陳中鈺,苑躍.1981—2013年四川省視程障礙類天氣現(xiàn)象分析[J].氣象科技,2018,46(5):958~964

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  • 收稿日期:2017-09-19
  • 定稿日期:2018-05-03
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  • 在線發(fā)布日期: 2018-10-31
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