近40年藏东南波堆藏布流域典型冰川变化特征

Glacier Change Characteristics in the Boduizangbo Basin of Southeastern Tibet over the Past 40 Years

  • 摘要: 基于1986—2023年多源卫星遥感数据,利用目视解译方法提取冰川面积,再结合地形和气候数据,分析近40 a藏东南波堆藏布流域三条典型现代冰川(则普冰川、朱西沟冰川和白玉沟冰川)变化特征及其影响因素。结果表明:三条冰川处于明显退缩状态,冰储量和物质平衡均处于减少和负平衡状态,冰川末端海拔高度也有明显提升;三条冰川低坡度面积在减少,高坡度面积在增加,2023年则普和白玉沟冰川低海拔(4000 m)以下的面积几乎为零;波堆藏布流域年平均气温与冰川面积相关性十分显著,两者均在1998年、2002年和2003年出现显著突变,气温升高可能是引起波堆藏布流域冰川变化的主要因素之一。

     

    Abstract: Based on the multi-source satellite remote sensing data from 1986 to 2023, glacier areas were extracted using visual interpretation. Combined with terrain and climate data, the variation characteristics and influencing factors of three typical modern glaciers (Zepu Glacier, Zhuxigou Glacier and Baiyugou Glacier) in the Boduizangbu Basin of southeastern Tibet over the past 40 years were analyzed. The results show that the three glaciers were in a state of obvious retreat, the ice storage and material balance were in a state of reduction and negative balance, and the altitude at the end of the glacier was also significantly improved. The low slope area of the three glaciers decreased, while the high slope area increased. In 2023, the area of the Zepu Glacier and Baiyugou Glacier below 4000 m elevation was nearly zero. The correlation between the annual average temperature and the glacier area in the Boduizangbu Basin was very significant. Both of them showed significant mutations in 1998, 2002 and 2003. The temperature rise may be one of the main factors causing the glacier change in the Boduizangbu Basin.

     

/

返回文章
返回