杨梅, 李岩瑛, 朱陵晶, 罗晓玲, 姜瑞, 聂鑫. 河西走廊东部1961—2017年不同等级冷空气时空变化及寒潮特征[J]. 沙漠与绿洲气象, 2022, 16(5): 87-93.
引用本文: 杨梅, 李岩瑛, 朱陵晶, 罗晓玲, 姜瑞, 聂鑫. 河西走廊东部1961—2017年不同等级冷空气时空变化及寒潮特征[J]. 沙漠与绿洲气象, 2022, 16(5): 87-93.
YANG Mei, LI Yanying, ZHU Lingjing, LUO Xiaoling, JIANG Rui, NIE Xin. Spatio-Temporal Variation of Cold Air in Different Levels and Cold Wave Characteristics During 1961-2017 over Eastern Hexi Corridor[J]. Desert and Oasis Meteorology, 2022, 16(5): 87-93.
Citation: YANG Mei, LI Yanying, ZHU Lingjing, LUO Xiaoling, JIANG Rui, NIE Xin. Spatio-Temporal Variation of Cold Air in Different Levels and Cold Wave Characteristics During 1961-2017 over Eastern Hexi Corridor[J]. Desert and Oasis Meteorology, 2022, 16(5): 87-93.

河西走廊东部1961—2017年不同等级冷空气时空变化及寒潮特征

Spatio-Temporal Variation of Cold Air in Different Levels and Cold Wave Characteristics During 1961-2017 over Eastern Hexi Corridor

  • 摘要: 基于河西走廊东部5个国家气象观测站1961—2017年的日最低气温,统计分析其5个等级冷空气的时空变化和降温幅度,应用NCEP月平均500 hPa位势高度场、风场得出寒潮显著极端年的特征。结果表明:(1)冷空气年均日数Ⅰ级最多,Ⅳ和Ⅴ级基本接近,Ⅲ级最少。空间分布Ⅰ级偏北沙漠区少、中部平原区多;其余四级分布均为偏北沙漠区偏多。时间分布Ⅱ、Ⅳ和Ⅴ级春季4—5月最多,夏季最少;Ⅲ级集中在夏季7—8月;Ⅰ级月、季出现频率接近,夏季8月略多。(2)年降温日数Ⅴ和Ⅳ级呈明显减少趋势,Ⅰ~Ⅲ级线性趋势不明显,其中Ⅰ和Ⅱ级略增多。年均降温频次的年代际差异不大,整体呈先降后升趋势。(3)平均降温幅度季节变化只有Ⅴ级明显,Ⅳ级相近,而Ⅰ~Ⅲ级最大分别出现在春季、秋季和夏季;Ⅴ级24、48、72 h最大降温幅度分别为9.9、12.2、14.3℃。(4)寒潮次数有12个极端年,寒潮显著偏多(少)年次数差异10月最大、夏季较小。河西走廊东部500 hPa位势高度场在显著偏多年为明显的西北气流控制,配合负距平中心,乌拉尔山脊前有极地干冷空气输送,有利于寒潮天气发生。偏少年以纬向平直西风气流为主,有明显的正距平高度,冷空气活动少,冷害天气不易发生。

     

    Abstract: Based on the daily minimum air temperature at five national meteorological observation stations over eastern Hexi Corridor during 1961-2017,the spatio-temporal variations and cooling ranges of cold air at five levels were statistically analyzed,and the characteristics of local extreme cold wave were obtained by applying monthly mean 500 hPa geopotential height field and wind field circulation data from NCEP.The results showed that:(1)The annual average days of cold air were the most in level Ⅰ,basically close in level Ⅴ and Ⅳ,and the least in level Ⅲ.For level Ⅰ,it was less in northern desert area and more in central plain area,and the other four levels were basically similar in which,the northern desert areas were more.The time distribution of level Ⅱ,Ⅳ and Ⅴ was the most in spring April-May but the least in summer;the Ⅲ level was concentrated in summer from July to August;the frequency of level Ⅰ was close in each month but slightly more in August.(2)The linear trend of annual cooling days decreased obviously in level V and Ⅳ,but showed weak linearity in level Ⅰ to Ⅲ with slightly increase in level Ⅰ and Ⅱ.The inter-decadal variation of the average annual cooling frequency was not significant,and the whole decreased first and then increased.(3)The seasonal variation of average cooling range was only obvious in level Ⅴ,similar to level Ⅳ,while the maximum cooling range of level Ⅰ to Ⅲ was in spring,autumn and summer,respectively;the maximum temperature drop of level Ⅴ at 24 h,48 h and 72 h was 9.9,12.2 and 14.3 ℃,respectively.(4)There were 12 extreme years in cold wave,the difference of cold wave days in more(less) years was the biggest in October but smaller in summer.During the positive-anomaly cold wave years,the 500 hPa geo-potential height field over eastern Hexi Corridor was controlled by northwest airflow with a negative anomaly height center,and the polar dry and cold air transport in front of the Urals Ridge was conducive to the occurrence of cold wave.During the negative-anomaly cold wave years,it was controlled in straight westerly with obvious positive anomaly height,as cold air activity was less,cooling disaster weather hardly occurred.

     

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