摘要
利用我国气象观测站1951-2000年降水、气温资料以及黄河上游有关水文测站1960-2003年的径流资料，分析了黄河上游和源区气候的年代际变化及其对径流变化的影响，并分析了黄河上游径流变化对华北水资源的影响。分析结果表明：黄河上游和源区降水从20世纪90年代有所减少，气温明显上升，导致了黄河源区和上游径流量锐减。黄河上游径流的减少是90年代黄河下游流量锐减、黄河断流天数增多的重要原因，并表明了黄河上游来水量的多少是影响华北地区水资源的重要原因。
The interdecadal variations of climate and their impact on the variations of runoff amount in the upper reach and source area of the Yellow River, and the impact of runoff amount variability in the upper reach of the Yellow River on water resources in North China are analyzed by using the observed data of precipitation and surface air-temperature in meteorological observational stations in China during 1951--2000 and the observed data of runoff amount in hydrological observational stations in the upper reach of the Yellow River during 1960--2003. The analyzed results show that from the 1990s, rainfall slightly decreased and surface air-temperature obviously increased in the upper reach and source area of the Yellow River, which have led to the significant decrease of runoff amount in the upper reach of the Yellow River. Moreover, the decrease of runoff amount in the upper reach of the Yellow River may be an important season of the significant decrease of runoff amount in the lower reach of the Yellow River and the increase of drying-up days of the Yellow River. This can show that the inputing water amount from the upper reach of the Yellow River is an important cause affecting the water resources in North China.
出处
《气候与环境研究》
CSCD
北大核心
2006年第3期245-258,共14页
Climatic and Environmental Research
基金
中国科学院重要创新项目KZCX3-SW-218
国家自然科学基金委员会重大研究计划重点项目40231005
关键词
黄河
气候
水文
水资源
the Yellow River, climate, hydrology, water resources
