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天山乌鲁木齐河源１号冰川１９５８－１９５９～１９９１－１９９２年度，以负物质平衡状态为主，累积负平衡量达８５１．９×１０４ｍ３，冰川平均亏损４５６２ｍｍ水层，与中亚山地冰川物质平衡的变化趋势相似，均是由夏季平均气温升高和年降水量减少引起的。分析１７ａ的物质平衡实测资料表明，净物质平衡与平衡线高度，以及平衡线高度与夏季平均气温和年降水量存在着密切关系，夏季平均气温变化１℃，平衡线高度变化１０２ｍ，年降水量变化１００ｍｍ，平衡线高度波动５８ｍ。
Tianshan Urumqi Heyuan Glacier No. 1 From 1958 to 1959 to 1991-1992, the main negative balance was the cumulative negative balance of 851.9 × 104 m3, the average glacier loss of 4562 mm, and the change of the mass balance of glaciers in Central Asia Similar trends are caused by an increase in average summer temperatures and a decrease in annual precipitation. The data of 17a shows that there is a close relationship between the net material balance and the equilibrium line height and the balance line height with the summer mean temperature and the annual precipitation. The average temperature changes in summer are 1 ℃, the height of the balance line is 102m, the annual precipitation Change 100mm, the balance line height fluctuation 58m.