中国东北近50年干旱发展及对全球气候变暖的响应
收稿日期: 2003-04-10
修回日期: 2003-07-20
网络出版日期: 2003-12-25
基金资助
国家重点基础研究发展规划项目 (G1999043405)
Arid Climate Trend over Northeastern China and Its Response to Global Warming
Received date: 2003-04-10
Revised date: 2003-07-20
Online published: 2003-12-25
Supported by
National Key Project for Basic Sciences, No.G1999043405
应用实测的降水、气温和土壤湿度资料，分析我国东北区 (含黑龙江、吉林、辽宁三省和内蒙古自治区的东部) 近50年干旱化的发展趋势。结果表明，用月平均气温和降水量的距平和均方差所构造的“大气干旱指数”以及土壤湿度都显示，近50年来整个东北区是向干旱发展的，1990年代中期以来这种干旱化趋势尤为明显；而东北西部亚干旱地区的干旱化相对更严重 (特别是内蒙古东部的北半部)。在亚干旱地区的气温和降水两个要素中，气温的升高对干旱化的作用可能更重要。在东北区的南部，近50年来的降水是略有增加，但仍有向干旱发展的趋势。这显然与全球气候变暖的大背景有关。为探讨东北区干旱的发展对全球气候变暖的响应，利用Jones等的1951~2000年全球平均气温资料和东北区25个站的大气干旱指数进行线性回归分析。结果表明，在全球平均温度上升1oC的情况下，中国东北区的干旱化程度要增加5~20%，最大的达到22%。这种形势应该引起我们的关注。
谢安,孙永罡,白人海 . 中国东北近50年干旱发展及对全球气候变暖的响应[J]. 地理学报, 2003 , 58(7s) : 75 -82 . DOI: 10.11821/xb20037s009
The station data, including precipitation, air temperature and soil humidity are employed to investigate the arid climate trend for the past 50 years over northeastern China. "Atmospheric drought index" is proposed based on monthly mean temperature and precipitation anomalies as well as mean variance. The variations in the index and soil humidity show that the arid situation gets deteriorated throughout the northeastern China, this arid trend is more significant since the mid-1990s, especially in semi-arid area located in northeastern Inner Mongolia. Air temperature increase plays a more important role than precipitation decrease does in terms of the formation of drought. Although rainfall has slightly increased over the southern part of northeastern China in recent 50 years, arid trend remains to be developing, which is obviously associated with global warming. The responses of aridity developing over northeastern China to the global warming are explored using linear regression analyses. The results show that under circumstance of global temperature increase by 1oC the aridity extent will rise 5-20%, its maximum will reach 22%.
[1] China Meteorological Administration. Climate Atlas of the People's Republic of China. Beijing: Cartographic Publishing House, 1979. 222-223.
[中央气象局. 中华人民共和国气候图集. 北京: 地图出版社, 1979. 222-223.]
[2] Li Baolin, Zhou Chenghu. Climatic variation and desertification in west sandy land of Northeast China Plain. Journal of Natural Resources, 2001, 16(3): 234-239.
[李宝林, 周成虎. 东北平原西部沙地的气候变异与土地荒漠化. 自然资源学报, 2001, 16(3): 234-239.]
[3] Li Shuai, Bai Renhai, Chen Li. A study on variation of summer rainfall and water level over Nen River and Songhua River valley. Heilongjiang Meteorology, 2002, (3): 7-11.
[李帅, 白人海, 陈莉. 嫩江、松花江流域夏季降水与水位变化分析. 黑龙江气象, 2002, (3): 7-11.]
[4] Qin Dahe (ed.). Appraisal on the Environment over Western China. Beijing: Science Press, 2002.
[秦大河 编. 中国西部环境演变评估. 北京: 科学出版社, 2002.]
[5] Wu Hongbao. Study on drought index over the southeastern China in summer. Quarterly Journal of Applied Meteorology, 2000, 11(2): 137-144.
[吴洪宝. 我国东南部夏季干旱指数研究. 应用气象学报, 2000, 11(2): 137-144.]
[6] Педъ Д А. О показателе засухи и избыточиого увлажпепия. Труды ГМЦ., 1975, 156: 19-38.
[7] Chen Liting, Sun Yuting et al. Climate and Agriculture of Heilongjiang Province. Beijing: Meteorology Press, 2000. 2-25.
[陈立亭, 孙玉亭 等. 黑龙江省气候与农业. 北京: 气象出版社, 2000. 2-25.]
[8] Wang Jingui, Xu Junqiang (eds). The Study of Short-range Climate over Northeast China. Beijing: Meterorology Press, 1998. 113-124.
[王锦贵, 许君强 主编. 东北短期气候研究. 北京: 气象出版社, 1998. 113-124.]
[9] IPCC. Climate change 2001: the scientific basis. In: Houghton J T, Y H Ding, D J Griggs et al. (eds.), Contribution of Working Group I to the Third Assessment Report of the Intergovernmental Panel on Climate Change. Cambridge, UK: Cambridge University Press, 2001. 944.
[10] Jones P D, New M Parker, D E Martin et al. Surface air temperature and its changes over the past 150 years. Reviews of Geophysics, 1999, 37: 173-199.
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