地球科学进展 ›› 2005, Vol. 20 ›› Issue (9): 1037 -1040. doi: 10.11867/j.issn.1001-8166.2005.09.1037

干旱气象研究 上一篇    下一篇

“环境蠕变”概念之我见
张 强,张 凯   
  1. 中国气象局兰州干旱气象研究所,甘肃省干旱气候变化与减灾重点实验室,甘肃 兰州 730020
  • 收稿日期:2004-08-16 修回日期:2005-03-14 出版日期:2005-09-25
  • 通讯作者: 张 强
  • 基金资助:

    国家科技部“西部开发科技行动”重大项目“祁连山空中云水资源开发利用研究”(编号:2004BA901A16)资助

DEFINITION OF ENVIRONMENTAL CREEPING

ZHANG Qiang; ZHANG Kai   

  1. Key Laboratory of Arid Climatic Changing and Reducing Disaster of Gansu Province, Institute ofArid Meteorology, China Meteorological Administration, Lanzhou 730020,China
  • Received:2004-08-16 Revised:2005-03-14 Online:2005-09-25 Published:2005-09-25

简要概述了“环境蠕变(Environmental Creeping)”这一新概念的由来,探讨了“环境蠕变”与全球变化的关系,对“环境蠕变”给出了一个相对比较明确的科学定义,并抽象和归纳出了“环境蠕变”的本质特征和科学内涵,最后指出了对待“环境蠕变”的科学态度。

“Environmental Creeping” was highly concerned by the international science fields and the political circles as a new science direction. It plays a very important role in global change. It is highly important that we should combine “Environmental Creeping” with global change. As a science problem, we should understand and develop it gradually. At present, it is the most initial problem that we should to define the conception of “Environmental Creeping” scientifically and definitely, and had better make clear the connotation and character of “Environmental Creeping” in the round. In order to explain the doubts, the author seriously considered this problem from the scientific point of view. Firstly, this paper briefly reviewed the origin of the new idea of “Environmental Creeping”, analyzed the relationship of “Environment Creeping” and Global change, and then, a more specific scientific notion was given. Secondly, the essence character and scientific meaning of “Environmental Creeping” were abstracted and concluded. At last, we pointed out the scientific attitude to “Environmental Creeping”.

中图分类号: 

[1] China Climate Change Group. China Climate Change Country Study[M].Beijing: Tsinghua University Press,2000. [中国气候变化国别研究组.中国气候变化国别研究[M].北京:清华大学出版社,2000.]
[2] Qin Dahe. Assessment on Environment in West China[M]. Beijing: Science Press,2002.[秦大河.中国西部环境演变评估[M].北京:科学出版社,2002.]
[3] Ding Yihui, Wang Shourong. Generality on Climate and Ecoenvironment in Northwest Region of China[M].Beijing: Meteorological Press,2001.[丁一汇,王守荣.中国西北地区气候与生态环境概论[M].北京:气象出版社,2001.]
[4] Shi Yafeng. The Effect of Climate Changes on the Water Resources in Northwestern and Northern China[M]. Jinan: Shandong Science and Technology Press,1995.[施雅风.气候变化对西北华北水资源的影响[M].济南:山东科学技术出版社,1995.]
[5] Acuna-Sota R, Stahle D W, Cleaveland M K, et al. Megadrought and megadeath in 16th century Mexico[J]. Emerging Infectious Diseases, 2002, 8(4):360-362.
[6] Schubert S D, Suarez M J, Pegion P J, Koster R D, et al. On the cause of the 1930s dust bowl[J].Science, 2004,303:1 855-1 859.

[1] 曲建升, 肖仙桃, 曾静静. 国际气候变化科学百年研究态势分析 *[J]. 地球科学进展, 2018, 33(11): 1193-1202.
[2] 史培军, 王爱慧, 孙福宝, 李宁, 叶涛, 徐伟, 王静爱, 杨建平, 周洪建. 全球变化人口与经济系统风险形成机制及评估研究[J]. 地球科学进展, 2016, 31(8): 775-781.
[3] 吴炳方, 邢强. 遥感的科学推动作用与重点应用领域[J]. 地球科学进展, 2015, 30(7): 751-762.
[4] 黄邦钦, 柳欣. 边缘海浮游生态系统对生物泵的调控作用[J]. 地球科学进展, 2015, 30(3): 385-395.
[5] 艾丽坤, 王晓毅. 全球变化研究中自然科学和社会科学协同方法的探讨[J]. 地球科学进展, 2015, 30(11): 1278-1286.
[6] 房启飞, 张虎权. 地球系统变化对叠层石衰减影响的研究综述[J]. 地球科学进展, 2014, 29(9): 1003-1010.
[7] 魏学琼, 叶瑜, 崔玉娟, 李蓓蓓, 袁存, 方修琦. 中国历史土地覆被变化重建研究进展[J]. 地球科学进展, 2014, 29(9): 1037-1045.
[8] 刘贤赵, 张勇, 宿庆, 田艳林, 全斌, 王国安. 现代陆生植物碳同位素组成对气候变化的响应研究进展[J]. 地球科学进展, 2014, 29(12): 1341-1354.
[9] 史培军, 孔锋, 叶谦, 汪明, 刘凯. 灾害风险科学发展与科技减灾[J]. 地球科学进展, 2014, 29(11): 1205-1211.
[10] 汪品先. 对地球系统科学的理解与误解——献给第三届地球系统科学大会[J]. 地球科学进展, 2014, 29(11): 1277-1279.
[11] WuGuoxiong,LinHai,ZouXiaolei,LiuBoqi,HeBian. 全球气候变化研究与科学数据[J]. 地球科学进展, 2014, 29(1): 15-22.
[12] 周广胜,何奇瑾. 生态系统响应全球变化的陆地样带研究[J]. 地球科学进展, 2012, 27(5): 563-572.
[13] 张俊辉,夏敦胜,张英,刘宇航. 中国泥炭记录末次冰消期以来古气候研究进展[J]. 地球科学进展, 2012, 27(1): 42-51.
[14] 曾庆存,林朝晖. 地球系统动力学模式和模拟研究的进展[J]. 地球科学进展, 2010, 25(1): 1-6.
[15] 崔胜辉,李方一,黄 静,于裕贤. 全球变化背景下的敏感性研究综述[J]. 地球科学进展, 2009, 24(9): 1033-1041.
阅读次数
全文


摘要