1954~2017a阿勒泰市春季各级别寒潮过程强度评估
Characteristics of Frequency, Intensity and Climate of Cold Wave in Altay 1954-2017a
DOI: 10.12677/CCRL.2020.94042, PDF,    科研立项经费支持
作者: 博尔楠:中国气象局乌鲁木齐沙漠气象研究所,新疆 乌鲁木齐;中亚大气科学研究中心,新疆 乌鲁木齐;赵江伟, 陈丽娟, 哈那提汗:阿勒泰地区气象局,新疆 阿勒泰
关键词: 寒潮过程标准化指数强度阿勒泰Cold Waves Process Standardized Index Intensity Altay
摘要: 利用阿勒泰基准气候站日最低气温资料,资料长度从1954年到2017年的春季,以日最低气温及其降温幅度为指标,计算寒潮过程单要素强度评估指标包括:寒潮降温幅度,最大24 h降温幅度,最大48 h降温幅度,最大72 h降温幅度,过程最低气温,过程最低气温距平;以寒潮综合强度指数IY评估各次寒潮天气过程,结果表明:1) 以寒潮天气过程降温幅度标准化指数IA为指标,强度从大到小排列前十位的过程一般寒潮和强寒潮过程各月分布比较均匀,特强寒潮过程全部现在3月。2) 以寒潮天气过程最大24 h、48 h和72 h降温幅度标准化指数I24 h、I48 h和I72 h为指标,强度从大到小排列前十位的寒潮过程中一般寒潮过程出现在3月的分别有2次、1次和4次,出现在4月的均为3次,出现在5月的分别有5次、6次和3次;强寒潮过程出现在3月的分别有6次、6次和5次,出现在4月的分别有2次、2次和3.5次,出现在5月的分别有2次、2次和1.5次;特强寒潮过程全部出现在3月。3) 以寒潮天气过程最低气温标准化指数ITD为指标,强度从大到小排列前十位的各级别寒潮过程全部出现在3月。以寒潮天气过程最低气温距平标准化指数IJP为指标,强度从大到小排列前十位的寒潮过程中一般寒潮过程中4次出现在4月,6次出现在5月;强寒潮和特强寒潮过程均有9次出现在3月,1次出现在4月。4) 以各级别寒潮过程强度综合评估指标IY为指标,强度从大到小排列前十位的一般寒潮过程3月只出现了1次,4次出现在4月,5次出现在5月;排列前十位的强寒潮过程中8次出现在3月,2次出现在4月;排列前十位的特强寒潮过程中9次出现在3月,1次出现在4月。5) 春季一般寒潮和强寒潮过程强度均为强度呈减弱的趋势,但不显著;而特强寒潮过程为强度减弱且显著。
Abstract: Based on the daily minimum temperature data of Altay reference climate station from 1954 to the spring of 2017, taking the daily minimum temperature and its cooling range as indexes, the single factor intensity evaluation index of cold wave process is calculated, that including cold wave cooling range, maximum 24 h cooling range, maximum 48 h cooling range, maximum 72 h cooling range, process minimum temperature and process minimum temperature anomaly. Evaluation of each cold wave weather process by cold wave comprehensive intensity index IY, the results are as follows: 1) Taking the cold wave weather process standardization index IA as the index, the process of ranking the top ten from large to small intensities generally distributes relatively evenly during each month during the general cold wave and strong cold wave, and all the extremely strong cold wave processes are in March. 2) Taking the cold wave weather process maximum 24 h, 48 h and 72 h standardization index I24 h, I48 h and I72 h as indicators, the general cold wave process occurred twice, once and 4 times in March respectively during the cold wave process of the top ten intensities from largest to smallest, all appeared in April for 3 times, and appeared in May for 5 times, 6 times and 3 times respectively, the strong cold wave process appeared 6 times, 6 times and 5 times in March respectively, and twice, twice and 3.5 times in April respectively, and there were twice, twice and 1.5 times in May respectively. The extremely strong cold wave process all appeared in March. 3) Taking the cold wave weather process minimum temperature standardized index ITD as an indicator, the top ten cold wave processes of all levels with intensity from large to small all appeared in March. Taking the cold wave weather process the lowest temperature anomaly standardized index IJP as an indicator, the general cold wave occurred 4 times in April and 6 times in May for the top ten cold waves with intensity from large to small, while strong cold waves process and super strong cold waves process all occurred 9 times in March and once in April. 4) Taking the comprehensive evalu-ation index IY of the cold wave process intensity of each level as the index, the general cold wave process with the intensity ranked in the top ten from largest to smallest occurred only once in March, 4 times in April, and 5 times in May, 8 times of the strong cold waves in the top ten appeared in March and twice in April, 9 times of the extremely strong cold waves in the top ten appeared in March and once in April. 5) The intensity of the general cold wave and strong cold wave in spring showed a weakening trend, but not significant, while the extra-strong cold wave process was weak and significant.
文章引用:博尔楠, 赵江伟, 陈丽娟, 哈那提汗. 1954~2017a阿勒泰市春季各级别寒潮过程强度评估[J]. 气候变化研究快报, 2020, 9(4): 380-393. https://doi.org/10.12677/CCRL.2020.94042

参考文献

[1] 李宪之. 东亚寒潮侵袭的研究: 中国近代科学论著专刊: 气象学(1919-1949) [M]. 北京: 科学出版社, 1955: 35-117.
[2] 刘传凤. 我国寒潮气候评价[J]. 气象, 1990, 16(12): 40-43.
[3] 丁一汇, 蒙晓. 一次东亚寒潮爆发后冷涌发展的研究[J]. 气象学报, 1994, 52(4): 442-451.
[4] 张培忠, 陈光明. 影响中国寒潮冷高压的统计研究[J]. 气象学报, 1999, 57(4): 493-501.
[5] 马杰. 全国大部分降水偏少两次寒潮影响明显[J]. 气象, 2009, 35(3): 120-123.
[6] 吴晓. 2008年初全国雨雪冰冻寒潮天气的OLR资料分析[J]. 气象, 2009, 35(4): 87-93.
[7] 王遵娅. 两次大范围寒潮侵袭我国[J]. 气象, 2009, 35(3): 124-125.
[8] Chan, J.C. and Li, C.Y. (2004) The East Asia Winter Monsoon. In: Chang, C.-P., Ed., East Asian Monsoon, Word Scientific, Singapore, 54-106.
[9] 丁一汇, 李巧苹, 柳艳菊, 等. 空气污染与气候变化[J]. 气象, 2009, 35(3): 3-14.
[10] 王遵娅, 丁一汇. 近53a年中国寒潮的变化特征及其可能原因[J]. 大气科学, 2006, 30(6): 1068-1076.
[11] 谭艳梅, 朱文娜, 张利平. 418寒潮天气过程中的锋生分析[J]. 沙漠与绿洲气象, 2009, 3(6): 13-16.
[12] 牟欢, 赵克明. 2010年春季新疆一次寒潮天气过程分析[J]. 沙漠与绿洲气象, 2011, 5(4): 35-39.
[13] 庄晓翠, 安冬亮, 张林梅, 等. 阿勒泰地区寒潮天气特征分析及预报[J]. 沙漠与绿洲气象, 2010, 4(1): 32-35.
[14] 曹兴, 毛炜峄, 尹冰霞, 等. 不同定义指标下的乌鲁木齐寒潮过程气候特征对比分析[J]. 沙漠与绿洲气象, 2017, 11(3): 31-37.
[15] 郑玉萍, 宫恒瑞. 乌鲁木齐市寒潮气候特征分析[J]. 沙漠与绿洲气象, 2015, 9(6): 56-61.
[16] 周雪英, 彭军, 段均泽, 等. 巴州一次寒潮降雪天气的特征分析[J]. 沙漠与绿洲气象, 2014, 8(3): 48-55.
[17] 张俊兰, 牟欢, 谢葭颖. 北疆寒潮天气分析及预报[J]. 沙漠与绿洲气象, 2015, 9(6): 11-18.
[18] 张家宝, 苏起元, 孙沈清, 等. 新疆短期天气预报指导手册[M]. 乌鲁木齐: 新疆人民出版社, 1986.
[19] 赵俊荣, 郭金强, 田惠萍. 2008年4月天山北坡一次强寒潮天气成因分析[J]. 气象与环境学报, 2010, 26(1): 54-58.
[20] 李海花, 刘大峰, 庄小翠, 等. 阿勒泰地区2008-04-17寒潮天气过程分析[J]. 陕西气象, 2009(5): 12-15.
[21] 张林梅, 庄小翠, 胡磊. 新疆阿勒泰地区一次强寒潮天气过程分析[J]. 干旱气象, 2010, 28(1): 71-75.
[22] 庄小翠, 安冬亮, 张林梅, 等. 阿勒泰地区寒潮天气特征分析及预报[J]. 沙漠与绿洲气象, 2010, 4(1): 32-35.
[23] 肉孜•阿基, 李如琦, 唐冶. 2011年初北疆强寒潮过程诊断分析[J]. 沙漠与绿洲气象, 2013, 7(3): 7-12.
[24] 李海燕, 杨霞, 张超. 新疆一次超极地寒潮天气分析[J]. 沙漠与绿洲气象, 2012, 6(5): 12-19.
[25] 陈豫英, 陈楠, 聂金鑫, 等. 2011年宁夏一次寒潮天气过程诊断[J]. 甘肃气象, 2012, 30(1): 88-93.
[26] 李效珍, 鲁巨, 刘建国. 大同地区秋季寒潮天气分型及预报[J]. 气象与环境科学, 2009, 32(增刊): 149-152.
[27] 高振荣, 刘晓云, 田庆明, 等. 甘肃河西地区一次强寒潮天气个例诊断分析[J]. 干旱气象, 2009, 27(1): 34-39.
[28] 孙玉莲, 任余龙, 韦伯龙, 等. 甘肃临夏地区2次沙尘寒潮天气成因对比[J]. 干旱气象, 2013, 31(1): 150-162.
[29] 赵玉广, 何丽华, 张南, 等. 河北省寒潮天气形势分析及预报[J]. 干旱气象, 2012, 30(1): 94-99.
[30] 毛炜峄, 白素琴, 陈鹏翔. 1951-2015年乌鲁木齐市降温过程频数及强度气候特征[J]. 气象, 2016, 42(11): 1374-1386.
[31] 毛炜峄, 陈颖. 1951-2015年乌鲁木齐市寒潮过程频数及强度气候特征[J]. 干旱气象, 2016, 34(3): 403-411.