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不同强度冷空气事件特征及对中国冬季温度的影响

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利用1979-2019年美国国家环境预报中心-国家大气研究中心再分析资料,采用冷空气爆发指数和二维阻塞高压指数,筛选出3类不同强度的冷空气事件:高-中纬(H-M)、高-低纬(H-L)、中-低纬(M-L)事件和乌拉尔山阻塞高压(UBH)事件,分析冬季3类冷空气事件的演变特征、UBH背景下冷事件的基本特征及其对中国的降温效果。结果表明,H-M和M-L事件的频次在2000年前呈下降趋势,M-L事件的强度总体上呈减小趋势。UBH背景下,66。1%的冷空气事件强度较强(冷空气爆发指数≥2),46。4%的冷空气事件持续时间为1 d,H-L事件的平均持续时间最长(3。4 d)。3类事件的冷空气通量在高纬欧亚大陆上空表现为由西伯利亚反气旋和东亚北部气旋组成的偶极型分布;阻塞高压影响下,偏北风加强,冷空气南下入口处的冷气团总量距平在事件开始前后最强达到110 hPa以上,50°N的温度负异常也受影响变得更加深厚,可以延伸到500 hPa以上;强的负热含量距平与强的地面温度异常对应,尤其在冷事件开始当天,50°N的负热含量距平远大于30°N。3类事件发生时,降温主要集中在中国北部和东部地区,H-L事件的降温效果最强,容易形成高纬至华南的穿透性冷空气事件。
Characteristics of cold air events with different intensities and cooling effects on winter temperature in China
Based on the National Centers for Environmental Prediction/National Center for Atmospheric Research reanalysis data from 1979 to 2019,the cold air outbreak index and two-dimensional blocking high index were used to screen out three types of cold air events with different intensities,i.e.high-to-middle latitudes(H-M),high-to-low latitudes(H-L),middle-to-low latitudes(M-L)events and Ural blocking high(UBH)events.The evolution characteristics of the three cold air events in winter,and the basic characteristics of the three cold events under the background of UBH and their cooling effect on China were analyzed,with the results that the frequency of H-M and M-L events showed a downward trend before 2000,and the intensity of M-L events generally showed a decreasing trend.Under the influ-ence of the blocking highs,66.1%of the cold air events were strong(cold air outbreaks index ≥2),the du-ration of 46.4%cold air events being 1 day,and the average duration of H-L events the longest(3.4 days).The cold airmass flux of the three types of events over the Eurasian continent at high latitudes showed a dipole distribution composed of the Siberian anticyclone and the North East Asian cyclone.Under the influence of the blocking highs,the northerly wind was strengthened,and the amount of cold airmass anomaly at the south entrance of cold air could reach more than 110 hPa before and after the onset days of the events,the negative temperature anomaly at 50°N was also affected more deeply,which could be extended above 500 hPa.The strong negative heat content anomaly corresponded to the strong tem-perature anomaly.On the onset day of a cold event,the negative heat content anomaly at 50°N was much larger than that at 30°N.When the three types of events occurred,the cooling regions were mainly con-centrated in the northern and eastern regions of China,with the cooling effect of H-L events being the strongest,for penetrating cold air events easy to form from high latitudes to southern China.

cold waveblocking high pressurepenetrating cold airSiberian high

鞠桂林、李旭、李艳、杜梦莹

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兰州大学大气科学学院,兰州 730000

寒潮 阻塞高压 穿透性冷空气 西伯利亚高压

2024

兰州大学学报(自然科学版)
兰州大学

兰州大学学报(自然科学版)

CSTPCD北大核心
影响因子:0.855
ISSN:0455-2059
年,卷(期):2024.60(6)