通过现代观测来检验湖面蒸发对中国干旱、半干旱区湖泊水位变化的影响(英文)

被引:2
作者
李育
王乃昂
李卓仑
马宁
周雪花
张成琦
机构
[1] CollegeofEarthandEnvironmentalSciences,CenterforHydrologicCycleandWaterResourcesinAridRe-gion,LanzhouUniversity
关键词
Holocene; lake level; lake evaporation; Qinghai Lake; Zhuye Lake; temperature; relative humidity;
D O I
暂无
中图分类号
P332 [水文观测(测验)]; P343.3 [湖泊、水库];
学科分类号
摘要
Qinghai Lake and Zhuye Lake, 400 km apart, are located in the northwest margin of the Asian summer monsoon. Water of these two lakes mostly comes from the middle and eastern parts of the Qilian Mountains. Previous studies show that the Holocene climate changes of the two lakes implied from lake records are different. Whether lake evaporation plays a role in asynchronous Holocene climate changes is important to understand the lake records. In this paper, we used modern observations beside Qinghai Lake and Zhuye Lake to test the impact factors for lake evaporation. Pan evaporation near the two lakes is mainly related to relative humidity, temperature, vapor pressure and sunshine duration. But tem-perature has different impacts to lake evaporation of the two lakes, which can affect Holocene millennial-scale lake level changes. In addition, differences in relative humidity on the millen-nial-scale would be more significant, which also can contribute to asynchronous lake records.
引用
收藏
页码:123 / 135
页数:13
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