地球科学进展 ›› 2013, Vol. 28 ›› Issue (11): 1257 -1268.

所属专题: 青藏高原研究——青藏科考虚拟专刊

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青藏高原东南缘丽江玉龙雪山气候变化特征及其对冰川变化的影响
辛惠娟 1, 何元庆 1, 张涛 1, 牛贺文 2, 杜建括 1   
  1. 1.中国科学院寒区旱区环境与工程研究所 冰冻圈科学国家重点实验室/玉龙雪山冰川与环境观测研究站,甘肃兰州730000; 2.兰州大学西部环境教育部重点实验室,西部环境与气候变化研究院,甘肃兰州730000
  • 出版日期:2013-11-10

The Features of Climate Variation and Glacier Response in Mt.Yulong, Southeastern Tibetan Plateau

Xin Huijuan 1, He Yuanqing 1, Zhang Tao 1, Niu Hewen 2, Du Jiankuo 1   

  1. 1.State Key Laboratory of Cryosphere Science,Yulong Glacial and Environmental Obsearvation Station, Cold and Arid Region Environment and Engineering Research Institution, Chinese Academy of Sciences, Lanzhou 730000, China; 2.Key Laboratory of Western China’s Environmental Systems (Ministry of Education), Research School of Arid; Environment and Climate Change, Lanzhou University, Lanzhou 730000, China
  • Online:2013-11-10 Published:2013-11-10
通过线性倾向估计、MannKendall突变检验、小波变换等方法,系统分析了青藏高原东南缘丽江玉龙雪山地区气候的变化趋势、突变和周期特征,在此基础上探讨了玉龙雪山白水1号冰川进退与该地区气候变化之间的关系。结果表明:①1951—2011年丽江气温、降水变化倾向分别为0.15℃/10 a和9.0 mm/10 a;年气温在1998年前后存在显著突变,年降水量突变不明显;干季气温与年气温主要表现为10~15 a的周期,湿季降水与年降水存在1个准10 a的变化周期。②1998年之前白水1号冰川末端进退受气温与降水共同控制,1998年之后则主要受控于气温;冷季缩短、气温增加是玉龙雪山东坡不同海拔高度气温变化的主要特征,其中冰川区增温值最大在2.2~2.5 ℃之间,冰川加速消融。
The Features of climate change in Mt.Yulong, southeasten Tibetan Plateau were analyzed using linear regression, MannKendall abrupt test and Morlet wavelet analyses. In addition, the relationship between glacier retreating (Baishui Glacier No.1) and climate warming wasalso analyzed in this study. The main results are showedas follow: ① The annual mean temperature, precipitation have an increasing trend, withinclination rates being 0.15℃/10a and 9.0 mm/10a;annual temperaturedramatically ascend in 1998 with the change values 0.7 ℃; Morlet waveletsin annual temperature andtemperature in dry season mainly have a 10 to 15year periods,while annual precipitation amount and the precipitation in rainyseason presented a quasi 10 year periods. ②Prior to 1998, the important meteorological factor influencing the change of Baishui Glacier No.1 are temperature and precipitation, while in the following years, temperature plays a more important role in affecting its retreat and advance; The main characteristic ofverticalclimate change in Mt. Yulong (1982/2009) is that the cold season shortens and temperature rises with elevation, and the maximal value of increased temperature in glacier zone is 2.2~2.5 ℃, resulting in greatly accelerated glacier ablation.
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