CAJ | 학술논문

以天山乌鲁木齐河源1号冰川1996／1997年度和1997／1998年度实测物质平衡资料为基础，利用等直线法计算出1号冰川年物质平衡分别为口-853.0mm和-789.9mm，相应的AAR值分别为0.25和0.33.自1959以来,1996／1997年度1号冰川物质负平衡值最大，1997／1998年度次之．根据该地区气温和降水记录资料分析，造成这种结果的主导因素是气温，尤其是夏季消融期气温,其次是降水．
이천산오로목제하원1호빙천1996／1997년도화1997／1998년도실측물질평형자료위기 출，이용등직선법계산출1호빙천년물질평형분별위구-853.0mm화-789.9mm，상응적AAR치분별 위0.25화0.33.자1959이래,1996／1997년도1호빙천물질부평형치최대，1997／1998년도차 지．근거해지구기온화강수기록자료분석，조성저충결과적주도인소시기온，우기시하계소융기기 온,기차시강수．
Based on the observation in 1996 / 1997 and 1997/1998, mass balances of the Glacier No.1 at the Headwaters of the Urumqi River were calculated as -853.0 mm and -789.9 mm. Since 1959, the negative value of mass balance in 1996/1997 has been the maximum, next to that in 1997/ 1998. By analyzing air temperature and precipitation in the region, it is found that the main factor resulting in this phenome- non is abnormal temperature, especially the abnormal summer temperature.