黔东南州近60年气温时空变化特征分析
Analysis of Temporal and Spatial Variation Characteristics of Temperature in Qiandongnan Prefecture in the Past 60 Years
DOI: 10.12677/CCRL.2020.95056, PDF,   
作者: 陈晓丹, 吴树炎*, 王敏敏, 李舒颖:贵州省黎平县气象局,贵州 黎平;蒋汉开:贵州黔东南气象局,贵州 凯里
关键词: 黔东南气温时空变化高温Qiandongnan Temperature Temporal and Spatial Variation Characteristics Hot Weather
摘要: 利用1960~2019年黔东南全州16个县市台站气温资料,使用气候变化分析方法如M-K突变检验、小波分析等,分析了黔东南州近60年来的气温时空变化特征。结果表明:黔东南州各县市年平均气温在14.7℃~18.5℃之间,全州年平均气温从1960年至今整体缓慢上升,M-K突变检验表明黔东南州气温突变点为2006年,且2009年以后气温的上升趋势十分显著。黔东南州年平均气温存在着准4年周期,在60年代有显著的3年左右的年际振荡周期,在1986~2010年有显著的4年振荡周期。黔东南州最冷月(1月)各县市月平均气温均在0℃以上,全州年平均最低气温 ≤ 0℃的日数在州西部为24~28 d,州南部仅为4 d左右;黔东南州最热月(7月)各县市月平均气温呈东部向西部递减的趋势,州西部较东部凉爽,北部较南部凉爽,全州年平均最高气温 ≥ 35℃日数南部年平均出现20 d以上,西部为0 d。
Abstract: With the temperature data of 16 stations of Qiandongnan from 1960 to 2019, using climate change analysis methods such as M-K test and wavelet analysis, the characteristics of spatial and temporal changes in temperature in Qiandongnan Prefecture in the past 60 years were analyzed. Results show that: The annual average temperature of Qiandongnan Prefecture is between 14.7˚C - 18.5˚C. The average annual temperature of the whole prefecture has been increasing slowly from 1960 to the present. The MK mutation test shows that the temperature mutation point of Qiandongnan Prefecture is 2006 and after 2009, the rising trend of temperature is very significant. The annual average temperature in Qiandongnan Prefecture has a quasi 4-year cycle. In the 1960s, there was a significant interannual oscillation cycle of about 3 years, and a significant 4-year oscillation cycle from 1986 to 2010. The coldest month (January) in Qiandongnan Prefecture, the monthly average temperature of all counties and cities is above 0˚C, and the number of days with the annual average minimum temperature ≤ 0˚C in the whole prefecture is 24 - 28 days in the western part of the state, and only about 4 days in the southern part; the hottest month in the state (July), the monthly average temperature of the counties and cities is decreasing from east to west. The western part of the state is cooler than the east, and the north is cooler than the south. In the southern of state, the number of days that the average annual maximum temperature of the whole state exceeds 35℃ is more than 20 days, while the west is 0 day.
文章引用:陈晓丹, 吴树炎, 王敏敏, 蒋汉开, 李舒颖. 黔东南州近60年气温时空变化特征分析[J]. 气候变化研究快报, 2020, 9(5): 508-514. https://doi.org/10.12677/CCRL.2020.95056

参考文献

[1] 秦大河, Thomasstocker. IPCC第五次评估报告第一工作组报告的亮点结论[J]. 气候变化研究进展, 2014, 10(1): 1-6.
[2] Oliver, J.E. (2013) Intergovernmental Panel in Climate Change (IPCC). Encyclopedia of Energy Natural Re-source & Environmental Economics, 26, 48-56. [Google Scholar] [CrossRef
[3] 任国玉, 徐铭志, 初子莹, 等. 近54年中国地面气温变化[J]. 气候与环境研究, 2005, 10(4): 717-727.
[4] 孙文, 范昊明. 全球变暖背景下松花江流域气温最新变化特征[J]. 水土保持研究, 2018, 25(3): 97-104.
[5] 丁丽佳, 王春林, 凌良新. 广东地区平均气温的时空变化特征[J]. 中国农业气象, 2011.
[6] 史佳良, 王秀茹, 李淑芳, 等. 近50年来河南省气温和降水时空变化特征分析[J]. 水土保持研究, 2017, 24(3): 151-156.
[7] 朱大运, 熊康宁, 董晓超. 贵州1960~2016年气温时空变化特征[J]. 水土保持研究, 2018, 25(4): 168-173.
[8] 刘晓冉, 李国平, 范广洲, 等. 西南地区近40a气温变化的时空特征分析[J]. 气象科学, 2008, 28(1): 30-36.
[9] 唐红忠, 白慧, 舒兴武, 等. 近51年贵州南部冬季气温气候特征及其变化规律[J]. 云南大学学报: 自然科学版, 2012, 34(S2): 374-380.
[10] 魏凤英. 现代气候统计诊断与预测技术[M]. 第2版. 北京: 气象出版社, 2016: 1-296.