自然资源学报 ›› 2004, Vol. 19 ›› Issue (3): 331-336.doi: 10.11849/zrzyxb.2004.03.009

• 气候变化 • 上一篇    下一篇

全球变暖对青藏高原腹地草地资源的影响

王谋1, 李勇1, 白宪洲1, 黄润秋2   

  1. 1. 成都理工大学地球科学学院,四川,成都 610059;
    2. 成都理工大学环境与土木工程学院 ,四川 成都 610059
  • 收稿日期:2003-10-13 修回日期:2004-01-27 出版日期:2004-06-25 发布日期:2004-06-25
  • 作者简介:王谋(1975~),男,博士生,从事生态环境及环境变化的研究。E-mail:edlgwm@21cn.com
  • 基金资助:

    自然科学基金“西部生态与环境”重大研究计划(90102002);国土资源部“温泉兵站”幅1:25万国土资源调查项目(200213000002)资助

The impact of global warming on vegetation resources in the hinterland of the Qinghai-Tibet Plateau

WANG Mou1, LI Yong1, BAI Xian-zhou1, HUANG Run-qiu2   

  1. 1. College of Earth Sciences, Chengdu University of Technology.Chengdu 610059,China;
    2. College of Environment and Civil Engineering, Chengdu University of Technology,Chengdu 610059,China
  • Received:2003-10-13 Revised:2004-01-27 Online:2004-06-25 Published:2004-06-25

摘要: 全球变化导致青藏高原腹地气候的暖干化趋势,也引起该区高寒草甸植被向高寒草原植被的退化。研究区内为高寒草甸一高寒草原过渡区,高寒草甸植被的退化速率为14.2km/10a,而相应地在退化区内生物总量亦呈下降趋势。气候暖干化是引起高原腹地植被退化的原因。而植被退化与区域生物总量的下降将成为影响该区环境自调能力和牧业经济发展的消极因素。

关键词: 全球变暖, 青藏高原腹地, 暖干化, 草地资源

Abstract: Global warming caused a dryer and warmer climate in the hinterland of the Qinghai-Tibet Plateau.Does it cause any responses from the plants ecology,and how?Based on field works and statistical data collected in 2002 and 2003,we basically concluded warming trend of the climate is the major reason for the succession devolution of alpine plants in the central part of the plateau.In the study area,it is specially causing a devolution from alpine Kobresia meadow to Alpine Stipa steppe at a rate of 14.2km/10a.Accordingly,the total biomass of the area is declining.With contrast to some relative researches,we basically concluded a dryer and warmer climate should take the responsibility for vegetation devolution accompanied with biomass decline in the area.Changes of the surface vegetation will be the negative factors influencing the capability of the environment self-adjustment and the development of the local economy.

Key words: global warming, hinterland of Qinghai-Tibet Plateau, warming trend, grassland resources