摘要
玛纳斯河的水量在20世纪90年代以来持续增加的背景上,在2003年出现了历史上罕见的汛期枯水现象。导致该现象的原因可能是频繁的天气过程导致高空温度不能稳步攀升,高山地区气温偏低使冰川和积雪不能大量消融。
On the background of continuing increase of annual discharge from 1990s,the discharge of the Manasi River was rather low during the flood season of 2003.It was due to the frequent climate system change,the temperature could not increase steadily, and snow and glacial couldn't melt greatly in the high mountains.
出处
《水土保持研究》
CSCD
2004年第4期198-199,共2页
Research of Soil and Water Conservation
基金
国家自然科学基金重大研究计划(90102016)资助
关键词
流量
气温
气候变化
玛纳斯河
discharge
temperature
climate change
the Manasi River
