Simulation of energy and water budget of Qinghai Lake, China

Qin Bo-qiang; Huang Qun

doi:10.1007/BF02844925

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Simulation of energy and water budget of Qinghai Lake, China

OriginalPaper | Updated：2023-05-16

- Simulation of energy and water budget of Qinghai Lake, China
- Simulation of energy and water budget of Qinghai Lake, China
- 海洋湖沼学报（英文） 1998年16卷第4期页码：289-297
- Affiliations：
  
  Nanjing Institute of Geography and Limnology
- Author bio：
- Funds：
  
  Project 49201005 supported by NSFC.
- DOI：10.1007/BF02844925
  中图分类号：
- 纸质出版：1998
- Accepted：
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Simulation of energy and water budget of Qinghai Lake, China[J]. 海洋湖沼学报（英文）, 1998,16(4):289-297.

Bo-qiang, Q., Qun, H. Simulation of energy and water budget of Qinghai Lake, China., Chin. J. Ocean. Limnol. 16, 289–297 (1998). https://doi.org/10.1007/BF02844925
Simulation of energy and water budget of Qinghai Lake, China[J]. 海洋湖沼学报（英文）, 1998,16(4):289-297. DOI： 10.1007/BF02844925.

Bo-qiang, Q., Qun, H. Simulation of energy and water budget of Qinghai Lake, China., Chin. J. Ocean. Limnol. 16, 289–297 (1998). https://doi.org/10.1007/BF02844925 DOI：

摘要

Abstract

Qinghai Lake

the biggest saline lake in China

is a mountainous lake located in the northeastern part of the Qinghai-Tibet Plateau

and has a closed drainage basin. Since the beginning of this century

the lake level has dropped significantly and the lake area has shrunk dramatically. Water balance analysis showed that the water budget deficit associated with decreased runoff was the main reason for the falling of lake level. In order to investigate the changes of hydrological conditions within the lake basin

a catchment model coupled with a lake thermodynamic model was developed to simulate the lake water balance and thermodynamics. The simulated water balance and lake level are quite consistent with observations. This model can be used to evaluate hydrological condition changes induced by external foreing such as climate changes.

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references

De Bruin, H. A. R., Wessels, H. R. A., 1988. A model for the formation and melting of ice on surface waters.Journal of Applied Meteorology 27: 164–173.

Glazovsky, N. F., 1990, A Concept on the resolving of the aral Crisis.Proceeding of the USSR Academy of Sciences (Geographical Series), No.4: 28–41. (In Russian)

Hostetler, S. W., Bartlein, P. J., 1990. Simulation of lake evaporation with application to modeling lake level variations of harney-malheur Lake, oregon.Water Resources Research 26: 2603–2612.

Leontyev, O. K., 1983. The Problem of the Aral Sea,The Journal of Mosow University (Geographical Series) 5: 46–51. (in Russian)

Qin, B., 1993. The Hydrological characteristics and water budget of Qinghai Lake drainage basin.Chinese Journal of Oceanography and Limnology 11 (4): 314–20.

Sevastyanov, D. V., Smirnova, N. P., 1986. Issyk-Kul Lake and the tendency of its natural development. Nauka. Leningrad, p. 256. (in Russian)

Shuttleworth, W. J., Gash, J. H. C., Lloyd et al., 1988. An integrated micrometeorological system for evaporation measurement.Agric. For. Meteorol. 43: 295–317.

Shouttleworth, W. J., Wallace, J. S., 1984. Evaporation from sparse crops-an energy combination theory.Q. J. R. Meteorol. Soc. 111: 839–855.

Zhao, R., 1984. The catchment hydrological models. Hydroelectric Press, Beijing, p. 214. (in Chinese)

Zhao, R., 1992. The Xin Anjiang model applied in China.Journal of Hydrology 135: 371–381.

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