Allen R G, Pereira L S, Raes D et al., 1998. Crop evapotranspiration: Guidelines for computing crop water requirements. FAO Irrigation and Drainage Paper 56. Rome: United Nations Food and Agriculture Organization.
An C B, Feng Z D, Barton L, 2006. Dry or humid? Mid-Holocene humidity changes in arid and semi-arid China. Quaternary Science Reviews, 25: 351-361.
An Z, Porter S C, Kutzbach J E et al., 2000. Asynchronous Holocene optimum of the East Asian monsoon. Quaternary Science Reviews, 19: 743-762.
Berger A, Loutre M F, 1991. Insolation values for the climate of the last 10 million years. Quaternary Science Reviews, 10: 297-317.
Bian Q, Liu J, Luo X et al., 2000. Geotectonic setting, formation and evolution of Qinghai Lake, Qinghai, China. Seismology and Geology, 22(1): 20-26. (in Chinese)
Chen F H, Yu Z C, Yang M L, 2008. Holocene moisture evolution in arid Central Asia and its out-of-phase relationship with Asian monsoon history. Quaternary Science Reviews, 27: 351-364.
Chen L H, Qu Y G, 1992. Water-land Resources and Reasonable Development and Utilization in the Hexi Region. Beijing: Science Press. (in Chinese)
Colman S M, Yu S, An Z et al., 2007. Late Cenozoic climate changes in China’s western interior: A review of research on Lake Qinghai and comparison with other records. Quaternary Science Reviews, 26: 2281-2300.
Cong Z, Ni G, Yang D et al., 2008. Evaporation paradox in China. Advances in Water Science, 19(2): 147-152. (in Chinese)
Farrera I, Harrison S P, Prentice I C et al., 1999. Tropical climates at the last glacial maximum: A new synthesis of terrestrial palaeoclimate data: I. Vegetation, lake-levels and geochemistry. Climate Dynamics, 15: 823-856.
Guo L, Guo Y, Luo X et al., 2009. Evaporation capacity and climatic changing characters in Hexi Corridor of Gansu Province in recent 48 years and the influencing factors. Acta Agriculturae Universitatis Jiangxiensis, 31(2): 375-380. (in Chinese)
Hack J J, Caron J, Yeager S et al., 2006. Simulation of the global hydrological cycle in the CCSM community atmosphere model version 3 (CAM3): Mean features. Journal of Climate, 19: 2199-2221.
Harrison S P, Digerfeldt G, 1993. European lakes as palaeohydrological and palaeoclimatic indicators. Quaternary Science Reviews, 12: 233-248.
Herzschuh U, 2006. Palaeo-moisture evolution in monsoonal Central Asia during the last 50,000 years. Quaternary Science Reviews, 25: 163-178.
Li Y, Li X, Cui B et al., 2010. Trend of pan evaporation and its impact factors over Qinghai Lake Basin from 1961 to 2007. Journal of Lake Science, 22(4): 616-624. (in Chinese)
Li Y, Morrill C, 2010. Multiple factors causing Holocene lake-level change in monsoonal and arid Central Asia as identified by model experiments. Climate Dynamics, 35: 1115-1128.
Li Y, Wang N, Cheng H et al., 2009a. Holocene environmental change in the marginal area of the Asian monsoon: A record from Zhuye Lake, NW China. Boreas, 38: 349-361.
Li Y, Wang N, Morrill C et al., 2009b. Environmental change implied by the relationship between pollen assemblages and grain-size in N.W. Chinese lake sediments since the Late Glacial. Review of Palaeobotany and Palynology, 154: 54-64.
Linacre E T, 1993. Data-sparse estimation of lake evaporation using a simplified Penman equation. Agric. & Forestry Meteor., 64: 237-256.
Linacre E T, 1994. Estimating U.S. Class A pan evaporation from few climate data. Water International, 19: 5-14.
Lister G, Kelts K, Chen K Z et al., 1991. Lake Qinghai, China: Closed basin lake levels and the oxygen isotope record for ostracoda since late Pleistocene. Paleogeography, Paleoclimatology, Paleoecology, 84: 141-162.
Liu X, Shen J, Wang S et al., 2007. Southwest monsoon changes indicated by oxygen isotope of ostracode shells from sediments in Qinghai Lake since the Late Glacial. Chinese Science Bulletin, 52: 539-544.
Mischke S, Kramer M, Zhang C J et al., 2008. Reduced early Holocene moisture availability in the Bayan Har Mountains, northeastern Tibetan Plateau, inferred from a multi-proxy lake record. Paleogeography, Paleoclimatology, Paleoecology, 267: 59-76.
Morinaga H, Itota C, Isezaki N et al., 1993. Oxygen-18 and carbon-13 records for the last 14 000 years from lacustrine carbonates of Siling-Co (lake) in the Qinghai-Tibetan Plateau. Geophysical Research Letters, 20: 2909-2912.
Morrill C, 2004. The influence of Asian summer monsoon variability on the water balance of a Tibetan lake. Journal of Paleolimnology, 32: 273-286.
Morrill C, Overpeck J T, Cole J E et al., 2006. Holocene variations in the Asian monsoon inferred from the geochemistry of lake sediments in central Tibet. Quaternary Research, 65: 232-243.
Pachur H J, Wunnemann B, Zhang H, 1995. Lake evolution in the Tengger Desert, northwestern China, during the last 40,000 years. Quaternary Research, 44: 171-180.
Penman H L, 1948. Natural evaporation from open water, bare soil and grass. Proceedings of the Royal Society of London, Series A: Mathematical and Physical Sciences, 193: 120-146.
Qin B Q, Yu G, 1998. Implications of lake level fluctuations at 6 ka and 18 ka in mainland Asia. Global and Planetery Change, 18: 59-72.
Shen J, Liu X Q, Wang S M et al., 2005. Palaeoclimatic changes in the Qinghai Lake area during the last 18,000 years. Quaternary International, 136: 131-140.
Shen S, Sheng Q, 2008. Changes in pan evaporation and its cause in China in the last 45 years. Acta Meteorologica Sinica, 66(3): 452-460. (in Chinese)
Street-Perrott F A, Grove A T, 1979. Global maps of lake-level fluctuations since 30 000 yr B. P. Quaternary Research, 12: 83-118.
Wang L J, 2003. Analysis and strategies of the water table drop of reason of the Qinghai Lake. Journal of Qinghai University, 21: 28-31. (in Chinese)
Xiao J L, Chang Z, Wen R et al., 2009. Holocene weak monsoon intervals indicated by low lake levels at Hulun Lake in the monsoonal margin region of northeastern Inner Mongolia, China. The Holocene, 19: 899-908.
Xiao J L, Wu J T, Si B et al., 2006. Holocene climate changes in the monsoon/arid transition reflected by carbon concentration in Daihai Lake of Inner Mongolia. The Holocene, 16: 551-560.
Xiao J L, Xu Q H, Nakamura T et al., 2004. Holocene vegetation variation in the Daihai Lake region of north-central China: A direct indication of the Asian monsoon climatic history. Quaternary Science Reviews, 23: 1669-1679.
Yin Y, Wu S, Zheng D et al., 2008. Radiation calibration of FAO56 Penman-Monteith model to estimate reference crop evapotranspiration in China. Agricultural Water Management, 95: 77-84.
Yu G, Xue B, Liu J et al., 2003. LGM lake records from China and an analysis of climate dynamics using a modelling approach. Global and Planetery Change, 38: 223-256.
Zhang H C, Peng J L, Ma Y et al., 2004. Late Quaternary palaeolake levels in Tengger Desert, NW China. Paleogeography, Paleoclimatology, Paleoecology, 211: 45-58.
Zhang P X, Zhang B Z, Yang W B, 1989. On the model of postglacial palaeoclimatic fluctuation in Qinghai Lake region. Quaternary Sciences, 1: 66-77. (in Chinese)
Zhao Y, Yu Z, Chen F H et al., 2008. Holocene vegetation and climate change from a lake sediment record in the Tengger Sandy Desert, Northwest China. Journal Arid Environments, 72: 2054-2064.
Zuo H, Li D, Hu Y et al., 2005. Characteristics of climatic trends and correlation between pan-evaporation and environmental factors in the last 40 years over China. Chinese Science Bulletin, 50: 1235-1241.