1958—2008年山西气温变化的特征及趋势研究

doi:10.11867/j.issn.1001-8166.2010.03.0264

地球科学进展 ›› 2010, Vol. 25 ›› Issue (3): 264 -272. doi: 10.11867/j.issn.1001-8166.2010.03.0264

苗爱梅 ¹,武捷 ²,贾利冬 ³

1.山西省气象台，山西太原 030006;2.山西省气象信息中心，山西太原 030006;3.山西省气象局，山西太原 030002 

收稿日期:2009-05-13 修回日期:2010-01-01 出版日期:2010-03-10
通讯作者: 苗爱梅 E-mail:mam1226@163.com
基金资助:
山西省科技攻关项目“基于GIS的极端气象灾害预警与评估集成系统”（编号：20090311083）资助.

The Research of Air Temperature Variation Characteristics and Trend during 1958-2008

Miao Aimei ¹, Wu Jie ², Jia Lidong ³

1.Shanxi Meteorological Observatory, Taiyuan030006, China；
2.Shanxi Meteorological Information Center, Taiyuan030006, China；
3.Shanxi Meteorological Bureau, Taiyuan030002, China.

Received:2009-05-13 Revised:2010-01-01 Online:2010-03-10 Published:2010-03-10
Contact: Miao aimei E-mail:mam1226@163.com
Supported by:

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利用山西省气象信息中心归档的109个站1958—2008年的原始气象记录月报表及其信息化产品资料，研究山西平均气温、平均最高、最低气温以及平均日较差的变化趋势和特点，结果表明：1958—2008年山西平均气温、平均最高、最低气温增暖趋势分别为0.306℃/10a、0.337℃/10a和0.363℃/10a，比全国同期平均增温速率高得多;冬、春、秋季增温趋势分别为0.46℃/10a、0.35℃/10a和0.26 ℃/10a，增温幅度明显高于全国，夏季增温幅度则低于全国;平均日较差：年和冬、夏季均为减小趋势，春、秋季则为弱的上升趋势;晋北不但是年和四季增温最明显的区域，也是平均日较差减小范围和幅度最大的区域，晋西南是一年四季平均日较差增大范围和幅度最大的区域，晋东南夏季降温趋势明显;城市热岛效应加强因素对中等以上城市季节平均温度上升的贡献在夏季最高，冬季最小。

关键词: 全球变暖, 山西区域, 气温, 变化特征

With the original meteorological record, monthly report and informationized manufacture data of 109 stations during 1958-2008 archived by Shanxi Meteorological Information Center, the authors studied the variation trend and characteristics of average air temperature, average maximum and minimum air temperature, and average daily range of air temperature in Shanxi, the results show that: during the resent 51a, the warming trend of average air temperature, average maximum and minimum air temperature separately was 0.306℃/10a,0.337℃/10a and 0.363℃/10a in Shanxi, which was much higher than that of the corresponding period of the whole nation; the warming trend in winter, spring and autumn separately was 0.46℃/10a、0.35℃/10a和0.26 ℃/10a, the warming range was obviously higher than that of the whole nation, though, the warming range in summer was lower than that of the whole nation; the average daily range: was on descending trend in winter, summer and the whole year without exception, while in spring and autumn it was on weak upward trend. North Shanxi is not only the area where the seasonal and annual warming is the most obvious, but also is the area where the decreasing scope and extent of average daily range are maximum, Southwest Shanxi is the area where the increasing scope and extent of average daily range are maximum all the year round, in summer the air temperature appeared obvious dropping trend in the southeast of Shanxi; The contribution that the enhancing factor of urban heat island effect made to the seasonal average air temperature rising of moderate cities and above, is the highest in summer, and the lowest in winter.

Key words: Global warming, Shanxi region, Air temperature, Variation characteristics

中图分类号:

P423

[1] Jones P D，Moberg A. Hemispheric and large-scale surface air temperature variations: An extensive revision and an update to 2001[J].Journal of Climate,2003,16:206-223.
[2] Li Kerang, Lin Xianchao,Wang Weiqiang. Long-term trend of temperature change of China over the last 40 years[J].Geographical Research,1990,9(4):26-37.[李克让,林贤超,王维强.近四十年来我国气温的长期变化趋势[J].地理研究,1990,9(4):26-37.]
[3] Song Lianchun. Spatial and temporal change of China surface air temperature over the past 40 years[J].Journal of Applied Meteorological Science,1994,5(1):119-124.[宋连春.近40 年我国气温时空变化特征[J].应用气象学报,1994,5(1):119-124.]
[4] Zhai Panmao, Ren Fumin. Changes in maximum and minimum temperatures of the past 40 years over China[J].Acta Meteorologica Sinica,1997,55(4):418-429.[翟盘茂,任福民.中国近四十年最高最低温度变化[J]. 气象学报,1997,55(4):418-429.]
[5] Chen Longxun, Zhu Wenqin. Study on climate change of China over the past 45 years[J].Acta Meteorologica Sinica,1998,56(3):257-271.[陈隆勋,朱文琴.中国近45年来气候变化的研究[J].气象学报,1998,56(3): 257-271.]
[6] Tu Qipu, Deng Ziwang, Zhou Xiaolan. Study on regional feature of China temperature variation[J].Acta Meteorologica Sinica,2000,58(3):288-296.[屠其璞, 邓自旺, 周晓兰. 中国气温异常的区域特征研究[J].气象学报,2000,58(3):288-296.]
[7] Sha Wanying , Shao Xuemei , Huang Mei. Temperature change since 1980s in China and it s effect on natural area boundary[J].Sciences in China (Series D),2002 ,32(4):317-326.[沙万英, 邵雪梅, 黄玫. 20 世纪80 年代以来中国的气候变暖及其对自然区域界线的影响[J].中国科学:D辑,2002,32(4):317-326.]
[8] Ren Guoyu, Xu Mingzhi, Chu Ziying, et al.Changes of surface air temperature in China during 1951-2004[J].Climatic and Environmental Research, 2005,10( 4):717-727.[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.]
[9] Tang Guoli, Ren Guoyu. Reanalysis of surface air temperature change of the last 100 years over China[J]. Climatic and Environmental Research,2005,10(4):791-797.[唐国利,任国玉.近百年中国地表气温变化趋势的再分析[J]. 气候与环境研究, 2005,10(4):791-797.]
[10] Qian Weihong, Fu Jiaolan, Zhang Weiwei, et al. Changes in mean climate and extreme climate in China during the last 40 years[J].Advances in Earth Science,2007,23(7):674-683.[钱维宏,符娇兰,张玮玮,等.近40年中国平均气候与极值气候变化的概述[J].地球科学进展,2007,23(7):674-683.]
[11] Wang Pengxiang,Yang Jinhu, Zhang Qiang,et al. Climate change characteristic of northwest China in recent half century[J].Advances in Earth Science,2007,23(6): 650-655.[王鹏祥,杨金虎,张强,等.近半个世纪来中国西北地面气候变化基本特征[J]. 地球科学进展, 2007,23(6):650-655.]
[12] Zhou Tianjun, Zhao Zongci. Attribution of the climate warming in China for the 20th century[J].Advances in Climate Change Research,2006, 2(1): 28-32.[周天军,赵宗慈. 20世纪中国气候变暖的归因分析[J]. 气候变化研究进展, 2006,2(1):28-32.]
[13] Pu Bing , Wen Xinyu , Wang Shaowu，et al. Diagnostic and modeling study of the two basic modes of surface air temperature and its variation in China[J].Advances in Earth Science,2007,23(5):456-467.[濮冰 ,闻新宇 ,王绍武,等.中国气温变化的两个基本模态的诊断和模拟研究[J]. 地球科学进展, 2007,23(5):456-467.]
[14] Jones P D , Hulme M. Calculating regional climatic time series for temperature and precipitation: Methods and illustrations[J].International Journal of Climatology,1996,16:361-377.
[15] Zhou Yaqing, Ren Guoyu. Identifying and correcting urban bias for regional surface air temperature series of North China over Period of 1961-2000[J].Climatic and Environmental Research,2005,10(4): 743-752.[周雅清,任国玉.华北地区地表气温观测中城镇化影响的检测和订正[J]. 气候与环境研究, 2005,10(4):743-752.]
[16] China Statistic Bureau. Population Data of China Towns and City Districts[M]. Beijing: China Statistic Press, 2002.[中国统计局. 中国乡、镇、街道人口资料[M].北京:中国统计局出版社,2002.]

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