期刊文献+

黄河源区生态环境变化与成因分析 被引量:122

Eco-environmental Changes and Causal Analysis in the Source Regions of the Yellow River
下载PDF
导出
摘要 以70年代、80年代和90年代3个时期的卫星影像资料为基础,结合野外调查,对70年代以来黄河源区生态环境演变过程及趋势进行了对比分析,并依据相同时期的气候变化、人为活动强度分析,对该区域生态环境变化的产生原因进行了探讨.研究结果表明,与70年代相比,80年代和90年代以高寒沼泽草甸、高寒草甸和高山草原化草甸为代表的主要生态体系均呈现明显退化,尤其是90年代中期以来,高寒草原与高寒草甸植被退化剧烈,荒漠化发展迅速。 Based on three phases of satellite image data and field investigation, the eco-environmental evolution processes since the 1970s were analyzed. Analyses and discussions were made in this paper aimed at the understanding of the trend and causes of eco- environment changes in the regions over the last 20 a. The causes responsible for the environmental changes in the regions were explored in accordance with climate change and human activity. It is found that the eco-environment in the source regions of the Yellow River markedly degraded during the period of the 1980s-1990s compared with the 1970s. Especially from the mid-1990s, high-cold grassland and high-cold meadow vegetations seriously degraded, together with rapid desertification. The area of vegetation degradation increased from 24.5% in the 1980s to 34.5% of the total area of grassland and high-cold meadow in the 1990s. The expanding rate of desertification increased from 3.96% in the 1980s to 34.72% in the 1990s. Climate in the regions is becoming dry and warm, and permafrost is gradually degrading. Air temperature in the source regions of the Yellow River has been rising since 1954. Permafrost environment of the regions altered markedly, with an expansion of thawed.area and an increase in seasona thawing depth. Degradation of Permafrost led to a decrease of soil moisture content in root zone and surface soil desertification. In spite of this, summer precipitation in the regions also showed a decreasing tendency. Such regional climate change is not favorable for the normal growth of vegetation and thus will be causing extensive vegetation degradation. At the statuse of present the seasonal distribution of rangelands is unbalanced and irrational use. Consequently, cold-season rangelands are seriously overgrazed and thus causing pasture degradation. In addition, rodent and insect damages in the headwaiers are serious, covering 6% - 21 % of the total rangeland area.
出处 《冰川冻土》 CSCD 北大核心 2000年第3期200-205,共6页 Journal of Glaciology and Geocryology
基金 中国科学院寒区旱区环境与工程研究所创新项目!(210042) 中国科学院"西部之光"支持项目 中国科学院特别支持项目!"冰冻
关键词 黄河源区 生态环境演变 气候变化 冻土退化 成因 source regions of the Yellow River eco-environmental evolution processes climate change permafrost degradation
  • 相关文献

参考文献13

  • 1吴波,慈龙骏.毛乌素沙地荒漠化的发展阶段和成因[J].科学通报,1998,43(22):2437-2440. 被引量:28
  • 2陈全功,草业科学,1998年,7卷,4期,44页
  • 3程国栋,地球科学进展,1998年,13卷,增刊,24页
  • 4杨朝飞,黄河断流与流域可持续发展.黄河断流生态环境影响及对策研讨会论文集,1997年,1页
  • 5席家治,黄河水资源,1997年,259页
  • 6程国栋,气候变化对中国积雪、冰川和冻土的影响评价,1997年,49页
  • 7季中淳,冰川冻土,1996年,18卷,增刊,274页
  • 8康兴成,冰川冻土,1996年,18卷,增刊,281页
  • 9赵林,多年冻土影响下的土壤特征、青藏高原综合观测研究年报,1996年,70页
  • 10赵秀峰,青藏高原综合观测研究年报,1996年,1页

二级参考文献5

共引文献27

同被引文献1740

引证文献122

二级引证文献2651

相关作者

内容加载中请稍等...

相关机构

内容加载中请稍等...

相关主题

内容加载中请稍等...

浏览历史

内容加载中请稍等...
;
使用帮助 返回顶部