地球科学进展 ›› 2007, Vol. 22 ›› Issue (4): 350 -356. doi: 10.11867/j.issn.1001-8166.2007.04.0350

所属专题: “沙尘天气追因、影响及治理”虚拟专刊

研究论文 上一篇    下一篇

中国北方沙尘灾害影响因子分析
范一大 1,2,史培军 1,周 涛 1,李仪 2   
  1. 1.北京师范大学资源学院,北京 100875;2.中国民政部国家减灾中心,北京 100053
  • 收稿日期:2006-06-27 修回日期:2007-02-16 出版日期:2007-04-10
  • 通讯作者: 范一大(1968-),男,内蒙古呼和浩特人,副研究员,博士,主要从事自然灾害与风险管理研究.E-mail:fanyida@ndrcc.gov.cn E-mail:fanyida@ndrcc.gov.cn
  • 基金资助:

    科技部社会公益项目“国家重大自然灾害风险管理及预警体系研究”(编号:2005DIB3J013);国家重点基础研究发展计划项目“干旱化及其阶段性转折对我国粮食、水和土地资源安全的影响及其适应对策”(编号:2006CB400505)共同资助.

The Impact Factor Analysis of Dust Storm Disaster in Northern China

FAN Yi-da 1,2, SHI Pei-jun 1, ZHOU Tao 1, LI Yi 2   

  1. 1.College of Resources Science and Technology, Beijing Normal University, Beijing 100875, China;2. National Disaster Reduction Center of China, Beijing 100053, China
  • Received:2006-06-27 Revised:2007-02-16 Online:2007-04-10 Published:2007-04-10

利用中国北方1951—2000年188个沙尘暴代表站的气象观测数据和1983—2000年EROS数据中心NDVI数据,对我国北方沙尘灾害的影响因子进行了分析。主要结论有:①在影响沙尘暴发生、发展、演化的自然因子中,植被覆盖度、降水、大风日数和温度起关键作用,夏季植被覆盖度对来年春季沙尘暴发生频次影响较大,降水和温度主要表现在对地表植被覆盖等与沙尘暴有关的地表参数的影响;②大风日数和温度是沙尘暴形成的动力因子,植被覆盖度和降水是阻力因子。沙尘暴日数和持续时间的变化,主要取决于动力因子与阻力因子的综合作用;③遏制沙尘灾害的治本办法,不在于治理沙尘暴本身,而在于消除产生土地退化、生态安全下降的社会原因,处理好发展与生态环境建设的关系。

Based on data (1951-2000) from the 188 meteorological observation stations and the NDVI data (1983-2000) from EROS data center from1983 to 2000, the authers analyzed the impact factors of dust storm in northern China, and arrived at the main conclusions as follows: (1) Among the natural factors which affect the occurrence, development and evolution of dust storm, vegetation coverage, precipitation, windy days and temperature play a critical role. The summer vegetation coverageaffects the occurrence frequency of the following spring season. Precipitation and temperature have direct impact on the dust storm related groundparameters such as vegetation coverage. (2) Windy days and temperature are composed of the impetus factors of dust storm, and vegetationcoverage and precipitation are the main resistance factors. The changes of the dust storm days and duration mainly depend on theintegrated affection of the impetus factors and the resistance factors. (3) The fundamental measures to reduce dust storm disaster is not to deal with dust storm itself, but to eliminate the social impact which caused land and ecological degradation and to achieve the harmony development among social, economic and eco-environmental construction.

中图分类号: 

[1]Hu Yinqiao, Y Mitsuta. Micrometeorological characteristics and local triggering mechanism of strong dust storm[J]. Scientia Atmosoherica Sinica,1997,21(5):581-589.[胡隐樵,光田宁.强沙尘暴微气象特征和局地触发机制[J]. 大气科学,1997,21(5):581-589.]
[2]Wang Shigong,Dong Guangrong, Chen Huizhong, et al. Advances in studying sand-dust storms of China[J].Journal of Desert Research,2000,20(4):350-356.[王式功, 董光荣, 陈惠忠,等.沙尘暴研究的进展[J]. 中国沙漠,2000,20(4):350-356.]
[3]Quan Linsheng, Shi Shaoying, Zhu Yafen, et al. Temporal-Spatial distribution characteristics and causes of dust-day in China[J].Acta Geographic Sinica,2001, 56(4):477-485.[全林生,时少英,朱亚芬,等.中国沙尘天气变化的时空特征及其气候原因[J]. 地理学报,2001,56(4):477-485.]
[4]Joseph P V, Raipal D K, Deka S N. “Andhi”, the convective dust storms of northwest India[J].Mausam,1980,31:431-442.
[5]McNaughton D L. Possible connection between anomalous anticyclones and sandstorms[J].Weather,1987,42(1):8-13.
[6]Liu Jingtao, Zheng Mingqian. The climatic characteristics of blank storm in the northern part of north China[J].Journal of Weather,1998, 24(2):39-44.[刘景涛,郑明倩. 华北北部黑风暴的气候学特征[J]. 气象,1998,24(2):39-44.]
[7]Gong Daoyi, Shi Peijun. Variability of summer rainfall over northern China and its association with thermal conditions of early stage underlying surface[J].Journal of Natural Resources,2001, 16(3):211-215.[龚道溢,史培军. 华北农牧交错带夏季降水变率及其与前期下垫面热力状况的关系[J]. 自然资源学报,2001,16(3):211-215.]
[8]Li Dongliang, Wang Tao, Zhong Hailing. Climatic cause of sand-dust storm formation in northern China and its trend forecast[J].Journal of Desert Research,2004,24(3):376-379.[李栋梁, 王涛, 钟海玲. 中国北方沙尘暴气候成因及未来趋势预测[J].中国沙漠,2004,24(3):376-379.]
[9]Mao Rui, Gong Daoyi, Fan Yida. Influences of synoptic variability on spring sand storm frequency in north China[J].Acta Geographica Sinica,2005,60(1):12-20.[毛睿,龚道溢,范一大.春季沙尘暴对华北沙尘暴频次的影响[J].地理学报,2005,60(1):12-20.]
[10]Shi Peijun, Yan Ping, Yuan Yi. Driving force analyses of the blown-sand activity in northern China[J].Quaternary Sciences,2001, 21(1):41-47.[史培军,严平,袁艺. 中国北方风沙活动的驱动力分析[J]. 第四纪研究,2001,21(1): 41-47.]
[11]Fan Yida, Shi Peijun, Wang Xiushan,et al.The analysis of typical dust storm in northern China by remote sensing[J].Advances in Earth Science,2002,17(2):289-294. [范一大,史培军,王秀山,等.中国北方典型沙尘暴的遥感分析[J].地球科学进展,2002,17(2): 289-294.]
[12]Xu Jiongxin. Physico-geographical factors for formation of sand-dust storms in Loess Plateau region: Factor analysis[J].Journal of Desert Research,2005,25(4):547-551. [许炯心.黄土高原地区沙尘暴形成的自然地理因素:Ⅰ影响因素分析[J]. 中国沙漠,2005,25(4):547-551.]
[13]Wang Tao, Chen Guangting, Zhao Halin, et al. Research progress on aeolian desertification process and controlling in north of China[J].Journal of Desert Research,2006,26(4):508-516.[王涛, 陈广庭, 赵哈林,等. 中国北方沙漠化过程及其防治研究的新进展[J]. 中国沙漠,2006,26(4):508-516.]
[14]Shao Yaping. Physics and Modeling of Wind Erosion[M]. The Netherlands: Kluwer Academic Publishers, 2000.
[15]Gillette D A, Adams J, Endo A, et al.Threshold Velocities for input of soil particles in the air by desert soils[J].Journal of Geophysical Research,1980, 85(c15):5 621-5 630.
[16]Zhang Zengxiang, Zhou Quanbin, Liu Bin,et al. Monitoring of the characters and ground-surface of dust storm area in north China remote sensing[J].Journal of Remote Sensing,2001,5(5):377-382.[张增祥,周全斌,刘斌,等.中国北方沙尘灾害特点及其下垫面状况的遥感监测[J]. 遥感学报,2001,5(5):377-382.]
[17]Zhang Guoping, Zhang Zengxiang, Liu Jiyuan. Spatial distribution of Aeolian erosion of soil and its driving factors in China[J]. Acta Geographica Sinica,2001,56(2):146-157.[张国平,张增祥,刘纪远. 中国土壤风力侵蚀空间格局及驱动因子分析[J]. 地理学报,2001,56(2):146-157.]
[18]Gu Wei, Cai Xuepeng, Xie Feng, et al. Study on relationship between begetation cover and distribution of days of sandstorm—Taking central and western Inner Mongolia for example[J].Advances in Earth Science,2002,17(2):273-277.[顾卫,蔡雪鹏,谢峰,等.植被覆盖与沙尘暴日数分布关系的探讨——以内蒙古中西部地区为例[J]. 地球科学进展,2002,17(2): 273-277.]
[19]Asrar G, Kanemasu E T, Jackson R D, et al. Estimation of total above-ground phytomass production using remotely sensed data[J].Remote Sensing of Environment,1985,17:211-220.
[20]Tucker C J, Holben B N, Elgin H J, et al. Remote Sensing of total dry matter accumulation in winter wheat[J].Remote Sensing of Environment,1981,11:171-190.
[21]Gutman G, Ignatov A. The derivation of the green vegetation fraction from NOAA/AVHRR data for use in numerical weather prediction models[J].International Journal of Remote Sensing,1998,19:1 533-1 543.
[22]Defries R S, Hansen M C, Townshend J R G. Global continuous fields of vegetation characteristics: A linear mixture model applied to multi-year 8km AVHRR data[J].International Journal of Remote Sensing,2000, 21(6/7):1 389-1 414.

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