首页|1961—2020年新疆区域性强冷空气及寒潮时空分布特征

1961—2020年新疆区域性强冷空气及寒潮时空分布特征

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选用1961—2020年新疆99个气象站气温、降水观测日资料,通过相关分析、线性趋势分析等方法,分析了新疆全年区域性强冷空气和寒潮的特征,并应用降水资料对新疆全年强冷空气和寒潮过程的干湿状况进行了识别。结果表明:(1)新疆区域性强冷空气和寒潮频次均有减少的趋势,在21世纪10年代更为显著,这种减少主要体现在秋季强冷空气与秋季寒潮频次的减少;(2)新疆寒潮在冬季3个月的发生频次较为接近;春季与秋季寒潮在11月最多,3月和4月次之;超强寒潮时间主要集中在冬季的12月和1月,强寒潮发生的频率则在2月最高;(3)新疆寒潮过程最低气温有所上升,降温幅度有所减小;过程平均降水量以及最大降水量自20世纪90年代以来较之前明显增加;新疆冬季区域性寒潮的降温幅度比春秋季区域性寒潮过程高1℃左右;(4)寒潮过程中最低气温和降水量最大中心基本出现在阿尔泰山及天山山区。新疆春秋季寒潮多为正常或干过程;冬季寒潮过程有76。4%为正常偏干,较湿和湿过程有85。7%集中在20世纪90年代以来。对寒潮过程干湿状况进行初步识别,有助于更全面地认识新疆寒潮的气候新特征,为防灾减灾服务;(5)冬季北疆及天山大多数站点是72h达到寒潮标准,而南疆则更多是在24h达到寒潮标准。
Spatial and temporal distribution characteristics of strong cold air and cold wave in Xinjiang from 1961 to 2020
Based on the temperature and precipitation observation daily data of 99 meteorological stations in Xin-jiang from 1961 to 2020,the characteristics of regional strong cold air and cold wave in Xinjiang were analyzed by using correlation analysis and linear trend analysis,as well as the dry and wet conditions of strong cold air and cold wave in Xinjiang were recognized using the precipitation data. The results showed that:(1) The fre-quency of regional strong cold air and cold wave in Xinjiang showed a decreasing trend,which was mainly mani-fested in the decrease of the frequency of strong cold air and cold wave in autumn,especially in 2010s. (2) The occurrence frequency of cold wave in Xinjiang was relatively close during the three months of winter. In spring and autumn the cold wave occurred most in November,followed by March and April. The occurrence time of super strong cold wave mainly concentrated in December and January,and the frequency of strong cold wave was the highest in February. (3) During the cold wave in Xinjiang,the minimum temperature increased and the cooling amplitude decreased,respectively,and both the mean and maximum precipitation increased significant-ly since the 1990s. Meanwhile,the cooling amplitude of the regional cold wave in Xinjiang in winter was about 1 ℃ larger than that in spring and autumn. (4) The minimum temperature and the maximum precipitation during cold wave process occurred in the Altai Mountains and Tianshan Mountains. In spring and autumn the cold wave in Xinjiang was usually normal or dry process,while in winter 76.4% processes were normal dry,and 85.7% of the wet and wet processes were concentrated in the 1990s. The preliminary identification of the dry and wet con-ditions of the cold wave was helpful to understand the new climate characteristics of the cold wave in Xinjiang more comprehensively and serve for disaster prevention and mitigation. (5) In winter,most stations in Northern Xinjiang and Tianshan Mountains reached the cold wave standard in 72 hours,while in Southern Xinjiang,most stations reached the cold wave standard in 24 hours.

Xinjiangregionalcold wavestrong cold airtemperature humidity characteristics

王蕊、林纾、卢国阳、刘丽伟、黄鹏程

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西安市环境监测站,陕西 西安 710000

兰州区域气候中心,甘肃 兰州 730020

新疆 区域性 强冷空气 寒潮 温湿特征

国家重点研发计划项目中国气象局兰州干旱气象研究所干旱基金项目

2018YFC1505601IAM202109

2024

冰川冻土
中国地理学会 中国科学院寒区旱区环境与工程研究所

冰川冻土

CSTPCD
影响因子:2.546
ISSN:1000-0240
年,卷(期):2024.46(3)
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