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《地理学报(英文版)》 2013-01
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Lake evaporation:A possible factor affecting lake level changes tested by mod-ern observational data in arid and semi-arid China

LI Yu, WANG Nai’ang, LI Zhuolun, MA Ning, ZHOU Xuehua, ZHANG Chengqi College of Earth and Environmental Sciences, Center for Hydrologic Cycle and Water Resources in Arid Re-gion, Lanzhou University, Lanzhou 730000, China  
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.
【Fund】: National Natural Science Foundation of China No.41001116
【CateGory Index】: P332;P343.3
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