气候与全球变化

蒙古高原中部气候变化及影响因素比较研究

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  • 1. 中国科学院地理科学与资源研究所,北京 100101;
    2. 中国科学院研究生院,北京 100049;
    3. 蒙古科学院地理所,乌兰巴托 210620;
    4. 日本国立环境研究所,茨城 305-8506
王菱(1940-),女,大连市人,研究员。多年从事农田蒸发、山地气候和气候变化研究。

收稿日期: 2007-03-27

  修回日期: 2007-07-13

  网络出版日期: 2008-01-25

基金资助

中国科学院知识工程创新项目(06W60000SZ,066U0401SZ).

Comparative studies on climate changes and influencing factors in central Mongolian Plateau Region

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  • 1. Institute of Geographic Sciences and Natural Resources Research, CAS, Beijing 100101,China;
    2. Graduate University of CAS, Beijing 100049,China;
    3. Institute of Geography of Mongolian Academy of Sciences,Ulaanbaatar 210620, Mongolia;
    4. National Institute for Environmental Studies, Ibaraki 305-8506,Japan

Received date: 2007-03-27

  Revised date: 2007-07-13

  Online published: 2008-01-25

Supported by

中国科学院知识工程创新项目(06W60000SZ,066U0401SZ).

摘要

利用蒙古国中部6个气象站1940~2004年和中国内蒙古自治区中部6个气象站1951~2004年的温度和降水资料,对两地的气候变化及其影响因素作了对比研究。结果表明:20世纪90年代与60年代相比,中国内蒙古6站平均升温1.35℃,蒙古国6站上升1.13℃,2000~2004年与60年代相比:中国内蒙古6站上升1.89℃,蒙古国则为1.37℃,中国内蒙古6站的升温速率高于蒙古国6站。对温度变化趋势作突变性检验,结果表明:温度发生突变时间是纬度较高地区早于纬度较低的地区,大城市早于中小城镇,城市化对温度变化影响比较明显。相对于温度变化,降水变化没有显著性的突变,但有周期变化,中国内蒙古降水变化有2.8年周期,蒙古国有4年、8年的周期,这可能因为中国内蒙古降水水汽主要来源于太平洋,而蒙古国降水的水汽主要来源于北冰洋。

本文引用格式

王 菱, 甄 霖, 刘雪林, Ochirbat Batkhishig, 王勤学 . 蒙古高原中部气候变化及影响因素比较研究[J]. 地理研究, 2008 , 27(1) : 171 -180 . DOI: 10.11821/yj2008010019

Abstract

Mongolian Plateau Region is facing many problems in environment and sustainable development including land degradation, soil erosion, water pollution, solid and hazardous waste disposal, land use conflicts and desertification, which have led to social consequences such as urban unemployment and poverty. Those issues are very serious in central part of the region where population density is relatively high and intensive economic activities have caused several problems such as climate change. The central Mongolian Plateau Region covers seven provinces (municipalities) of Mongolia including Selenge, Darhan-Uul, Ulaanbaatar, Govisumber, Tov, Dundgovi and Dornogovi and four sub-provinces of Inner Mongolian Autonomous Region of China like Huhhot, Baotou, XilinGol, and Ulan Qab. The study aims at comparative analysis of climate changes, impacts on major economic activities and affecting factors in Mongolia and Inner Mongolia using temperature and precipitation data extending from 1940 to 2004 from six stations of Mongolia and 1951~2004 from six stations of Inner Mongolia of China. The results show that in comparison with temperature data in the 1960s, the average temperature has risen by 1.35℃ in the 1990s in Inner Mongolia of China, while it is 1.13℃ in Mongolia. In the period of 2000-2004, the average temperature increase was 1.89℃ in Inner Mongolia and 1.37℃ in Mongolia in comparison with the 1960s, showing a faster temperature increase in Inner Mongolia than that in Mongolia. Mutation test of the changing trend of temperature indicates that temperature mutation usually occurs in the areas with high latitude followed by those of low latitude, and big cities followed by small and medium-sized towns. However, significant change of precipitation was not observed, but periodic changes instead. For instance, duration of precipitation in Inner Mongolia is 2.8 years, while it is 4 and 8 years in Mongolia, and those results reach 95% level of correction test. The climate change has brought about significant impacts on agricultural production, livestock raising and environment, which have been considered as important components of sustainable development of the region in a long run. The results are significant for understanding interaction between climate change, impacts and driving factors, and identifying most important areas for policy intervention, and finally for sustainable use and management of fragile natural resources.

参考文献


[1] 叶宝明.我国东北与蒙古国铁路通道建设研究.世界地理研究, 2004,13(2):26~33.

[2] 秦大河,陈宜瑜,李学勇 主编.中国气候变化与环境演变:上卷.北京:科学出版社,2005.1~200.

[3] 秦大河,陈宜瑜,李学勇 主编.中国气候变化与环境演变:下卷.北京:科学出版社,2005.1~397.

[4] 陈隆勋,周秀骥,李维亮.中国近80 年来气候变化特征及其形成机制.气象学报,2004,62(5):634~644.

[5] 陈素华,杨丽桃.气候变暖与内蒙古农业的发展.内蒙古气象,2001,(1):24~25.

[6] 白美兰.内蒙古东部近54年气候变化对生态环境演变的影响.气象,2006,(6)31~36.

[7] 路云阁,李双成,蔡运龙.近40年气候变化及其空间分异的多尺度研究——以内蒙古自治区为例.2004,24(4):432~438.

[8] 曹宇,欧阳华,肖笃宁,等.额济纳天然绿洲景观变化及其生态环境效应.地理研究,2005,24(1)131~139.

[9] 许炯心.土地利用变化对鄂尔多斯高原周边地区沙尘暴的影响.地理研究,2004,23(4)463~468.

[10] Tuvdendorj D.Dust storms over the territory of Mongolia.Thesis for the Ph.D. in Geography,Moscow,1974,190.

[11] Natsagdorj L,Jugder D,Chung Y S.Analysis of dust storms observed in Mongolia during 1937~1999.Atmospheric Environment,2003,(9-10):1401~1411

[12] S GLi, Asanuma J,Eugster W,at al.Net ecosystem carbon dioxide exchange over grazed steppe in central Mongolia,Global Change Biology,2005,11(1):1941~1955.

[13] Oyun D,Batbuyan G,Enkhzaya D.Mongolian Statistical Yearbook 2004,Ulaanbaatar:National Statistical Office of Mongolia,2005.87.

[14] 内蒙古自治区统计局.内蒙古统计年鉴2005.北京:中国统计出版社,2005.507~510.

[15] 任国玉,郭军,徐铭志.近50 年中国地面气候变化基本特征.气象学报,2005,63(6),944~953.

[16] Robert T Watson,Daniel L Albritton,Terry barker,et al.Climate Change 2001:Synthesis Report .Cambridge:Cambridge University Press,2001.1~46.

[17] 王菱,谢贤群,李运生,等.中国北方地区40年来湿润指数和干湿带界线的变化.地理研究,2004,23(1):45~54.

[18] 黄嘉佑 编著.气象统计分析与预报方法.北京:气象出版社,2004.215~226.

[19] 魏风英 编著.现代气候统计诊断与预测技术.北京:气象出版社,1999.35~89.

[20] 丁一汇,张锦,徐影,等. 气候系统的演变及其预测. 北京:气象出版社,2003.137.

[21] 高学杰, 赵宗慈, 丁一汇,等. 温室效应引起的中国区域气候变化的数值模拟,第二部分: 中国区域气候的可能变化. 气象学报,2003,61(1):29~38.

[22] 赵宗慈, 王绍武, 徐影,等. 近100 年我国地表气温趋势变化的可能原因分析. 气候与环境研究, 2005,10(4):808~817.

[23] 林学椿, 于淑秋. 北京地区气温的年代际变化和热岛效应.地球物理学报,2003,48(1):39~45.

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