首页 | 本学科首页   官方微博 | 高级检索  
     

蒙古高原东部和南部气候要素变化特征及其生态环境影响分析
引用本文:包光,刘禹,刘娜,王伟平. 蒙古高原东部和南部气候要素变化特征及其生态环境影响分析[J]. 地球环境学报, 2013, 0(5): 1444-1449
作者姓名:包光  刘禹  刘娜  王伟平
基金项目:陕西省自然科学基础研究计划项目(2014JQ5192);国家自然科学基金项目(41301101);黄土与第四纪地质国家重点实验室开放基金项目(SKLLQG1302);宝鸡文理学院重点项目博士启动基金(ZK11063)
摘    要:使用线性回归、趋势倾向性和空间相关等方法对比分析内蒙古辖区蒙古高原东部呼伦贝尔与南部额济纳旗地区器测时段气候变化特征。结果表明,呼伦贝尔与额济纳旗两地器测时段全年和生长季(6—9 月)平均温度增温显著,降水无显著共同变化,区域暖干化趋势明显。年径流总量变化、空间相关结果和周期分析显示,两地气候干湿变化具有同步趋势。全球变暖背景条件下,内蒙古东部沙地樟子松和西部胡杨面临着相近的气候环境与人类活动双重压力。

关 键 词:气候变化;温度;降水;径流;树轮重建;蒙古高原
收稿时间:2013-07-04

Characteristics of climate changes during the instrumental period in the easternand southern Mongolian Plateau and their ecological-environmental effects
BAO Guang,LIU Yu,LIU Na and WANG Wei-ping. Characteristics of climate changes during the instrumental period in the easternand southern Mongolian Plateau and their ecological-environmental effects[J]. Journal of Earth Environment, 2013, 0(5): 1444-1449
Authors:BAO Guang  LIU Yu  LIU Na  WANG Wei-ping
Affiliation:Shaanxi Key Laboratory of Disaster Monitoring and Mechanism Simulation, School of Geography and Environment,Baoji University of Arts and Sciences, Baoji 721013, China;State Key Laboratory of Loess and Quaternary Geology,Institute of Earth Environment, Chinese Academy of Sciences, Xi''an 710075, China,State Key Laboratory of Loess and Quaternary Geology,Institute of Earth Environment, Chinese Academy of Sciences, Xi''an 710075, China,Shaanxi Key Laboratory of Disaster Monitoring and Mechanism Simulation, School of Geography and Environment,Baoji University of Arts and Sciences, Baoji 721013, China and Baoji Environmental Monitoring Station, Baoji 721006, China
Abstract:Characteristics of climate changes in the Hulun Buir region and Ejina Banner during theinstrumental period, Inner Mongolia, were analyzed by the methods of linear regressions, trendsand spatial correlations. Our results indicated that significant warming trends existed in annual andgrowing seasonal mean temperatures in both regions, while no significant common trends existed inprecipitation. Variations of four annual runoff series, results of spatial correlations and period analysesshow a synchronous trend in wet and dry climate conditions existed in the eastern and southernMongolian Plateau. The effects of climate-related environmental pressure and human activities stresson the forest in the eastern and western Inner Mongolia are still serious under the global warmingbackground.
Keywords:climate change   temperature   precipitation   runoff   tree-ring reconstruction   Mongolian Plateau
点击此处可从《地球环境学报》浏览原始摘要信息
点击此处可从《地球环境学报》下载全文
设为首页 | 免责声明 | 关于勤云 | 加入收藏

Copyright©北京勤云科技发展有限公司  京ICP备09084417号