1979~2019年我国西南地区高温热浪时空分布特征研究
Study on Spatiotemporal Distribution Characteristics of High Temperature and Heat Waves in Southwest China from 1979 to 2019
摘要: 在全球变暖的大背景下,极端暖事件发生越来越频繁。为了进一步研究西南地区高温热浪时空分布特征规律,利用欧洲中期天气预报中心(ECMWF)的1979至2019年夏季的温度数据资料,运用趋势分析和Mann-Kendall检验等气候诊断方法,对西南地区高温热浪的时空分布特征进行研究,结果表明:41年来,高温热浪频次、持续时间和强度均在总体上呈现出线性增加的趋势,其速率分别为0.09次/10a、0.37 d/10a、0.44℃∙d。从突变情况看,2013年以前,高温热浪频次、持续时间和强度表现出增加趋势,但增加趋势不显著;2013年以后,高温热浪频次、持续时间和强度呈现出显著增加趋势;高温热浪频次、持续时间和强度在空间上的分布大致呈现东南多西北少的特征。高温热浪多发地区集中在研究区域中东部,而四川西部、云南西南部很少发生高温热浪事件;研究区域高温热浪频次、持续时间和强度除了云南西部和四川西部呈减少或不变趋势,其他地区都呈增加趋势,研究区域的中部地区增加趋势更大,通过0.05显著性检验的区域也集中在中部。
Abstract: In the context of global warming, extreme warming events occur frequently. In order to further study the spatial and temporal distribution characteristics of heat wave in southwest China, in this paper, linear trend analysis and Mann-Kendall test are used to study the spatial and temporal distribution of heat waves in southwest China. The 1979-2019 summer temperature data of European Centre for Medium-Range Weather Forecasts (ECMWF) are used. The following conclusions are drawn: Over the past 41 years, the frequency, duration and intensity of heat waves have shown a general trend of linear increase, with the rates of 0.09 times/10a, 0.37 d/10a and 0.44˚C∙d, respectively. From the mutation situation, before 2013, the frequency, duration and intensity of heat waves showed an increasing trend, but the increasing trend was not significant. After 2013, the frequency, duration and intensity of heat waves showed a significant increase trend. The spatial distribution of the frequency, duration and intensity of heat waves is more in the southeast and less in the northwest. The heat waves areas were concentrated in the central and eastern part of the study area, while the hot and heat wave events were rare in western Sichuan and southwestern Yunnan. Except for western Yunnan and western Sichuan, the frequency, duration and intensity of heat waves in the study area all showed an increasing trend. The central region of the study area had a larger increasing trend, and the regions that passed the 0.05 significance test were also concentrated in the central region.
文章引用:张月, 肖天贵, 曾珏桃, 杜宇. 1979~2019年我国西南地区高温热浪时空分布特征研究[J]. 自然科学, 2020, 8(4): 207-219. https://doi.org/10.12677/OJNS.2020.84027

参考文献

[1] IPCC/Climate Change 2013: The Physical Science Basis.
[2] Erdenebat, E. and Sato, T. (2016) Recent Increase in Heat Wave Frequency around Mongolia: Role of Atmospheric Forcing and Possible Influence of Soil Moisture Deficit. Atmospheric Science Letters, 17, 135-140. [Google Scholar] [CrossRef
[3] 沈皓俊, 游庆龙, 王朋岭, 等. 1961-2014年中国高温热浪变化特征分析[J]. 气象科学, 2018, 38(1): 28-36.
[4] 张平, 延军平, 李英杰, 唐宝琪, 王文静. 1960-2015年两广地区夏季高温热浪变化特征[J]. 浙江大学学报(理学版), 2018, 45(1): 73-81.
[5] 李双双, 延军平, 杨赛霓, 胡书山, 赵怡. 1960-2016年秦岭–淮河地区热浪时空变化特征及其影响因素[J]. 地理科学进展, 2018, 37(4): 504-514.
[6] 程迪, 王咏薇, 刘寿东, 肖帆. 1959-2012年夏季珠三角地区高温热浪的时空分布特征及其城市热岛效应的影响分析[J]. 科学技术与工程, 2019, 19(1): 273-283.
[7] 董晓晓, 武炳义. 江淮地区夏季高温事件与北极冷异常的动力联系[J]. 应用气象学报, 2019, 30(4): 431-442.
[8] 刘嘉慧敏, 郑然, 娄盼星, 梁绵. 2017年7月陕西高温热浪天气成因及前期信号初探[J]. 干旱气象, 2019, 37(2): 233-242.
[9] You, Q.L., Jiang, Z.H., Lei, K., et al. (2016) A Comparison of Heat Wave Climatologies and Trends in China Based on Multiple Definitions. Climate Dynamics, 1, 15. [Google Scholar] [CrossRef
[10] 叶殿秀, 尹继福, 陈正洪, 郑有飞, 吴荣军. 1961-2010年我国夏季高温热浪的时空变化特征[J]. 气候变化研究进展, 2013, 9(1): 15-20.
[11] 魏风英. 现代气候统计诊断与预测技术[M]. 北京: 气象出版社, 1999.
[12] 唐共地, 包赢. 基于有序聚类分析法和Mann-Kendall法的水沙系列突变点研究[J]. 江淮水利科技, 2015(6): 35-37.
[13] 谈建国, 郑有飞, 彭丽, 等. 城市热岛对上海夏季高温热浪的影响[J]. 高原气象, 2008, 27(S): 144-149.
[14] 陈敏, 耿福海, 马雷鸣, 等. 近138年上海地区高温热浪事件分析[J]. 高原气象, 2013, 32(2): 597-607.
[15] 张志薇, 王式功, 尚可政. 等. 华中地区近50年高温事件及大气环流成因分析[J]. 兰州大学学报(自然科学版), 2011, 47(2): 50-55.