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《Journal of Glaciology and Geocryology》 1987-04
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The Relationship Between Glacial Mass Balance Equilibrium Line and Climate

Yao Tandong (Lanzhou Institute of Glaciology and Geocryology, Chinese Academy of Sciences)  
The internal relationship and external characteristics of Glacier No.l are analysed in the present paper on basis of the measured and interpolated data.It is found from the analysis that the glacial equilibrium line variation (rise and drop) not only indicates the increase and decrease of mass balance,but also reveals different feedback mechnisms of glacial shape and surface albedo with the positive feedback accompanying equilibrium line drop and the negative feedback accompanying the rise. The relationship between the equilibrium line, precipitation and temperature shows that the stability of Glacier No.l is relatively high, compared with marintime glaciers and that therefore the glacier can reach its stable state with a relatively small accumulation area.That is to say, the glacier is slow in response to climate fluctuations, especially to temperature fluctuations.So equilibrium line equations have been derived for Glacier No-1 under different states,relating to temperature and precipitation.
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