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    藏东南则隆弄冰川运动速度长时间季节性变化规律

    薛泽远 范宣梅 邓宇 蒋力洋

    薛泽远, 范宣梅, 邓宇, 蒋力洋, 2026. 藏东南则隆弄冰川运动速度长时间季节性变化规律. 地球科学, 51(4): 1358-1370. doi: 10.3799/dqkx.2025.244
    引用本文: 薛泽远, 范宣梅, 邓宇, 蒋力洋, 2026. 藏东南则隆弄冰川运动速度长时间季节性变化规律. 地球科学, 51(4): 1358-1370. doi: 10.3799/dqkx.2025.244
    Xue Zeyuan, Fan Xuanmei, Deng Yu, Jiang Liyang, 2026. Long-Term and Seasonal Variations of Glacier Velocity in Zelongnong, Southeast Tibet. Earth Science, 51(4): 1358-1370. doi: 10.3799/dqkx.2025.244
    Citation: Xue Zeyuan, Fan Xuanmei, Deng Yu, Jiang Liyang, 2026. Long-Term and Seasonal Variations of Glacier Velocity in Zelongnong, Southeast Tibet. Earth Science, 51(4): 1358-1370. doi: 10.3799/dqkx.2025.244

    藏东南则隆弄冰川运动速度长时间季节性变化规律

    doi: 10.3799/dqkx.2025.244
    基金项目: 

    国家杰出青年科学基金项目 42125702

    四川省重大科技专项项目 2024ZDZX0020

    科学探索奖,强震和极端气候作用下青藏高原巨灾风险预测 2027-2023

    详细信息
      作者简介:

      薛泽远(2001-),男,硕士研究生,主要从事冰川地质灾害研究.ORCID:0009-0008-4273-2855. E-mail:849814088@qq.com

      通讯作者:

      范宣梅(1981-),女,博士,研究员.E-mail: fxm_cdut@qq.com

    • 中图分类号: P343.6; TP79

    Long-Term and Seasonal Variations of Glacier Velocity in Zelongnong, Southeast Tibet

    • 摘要:

      研究冰川运动速度对于理解高寒山区冰流的响应机制具有重要意义.然而在藏东南地区,由于时间和空间上的限制,许多冰川的运动研究仍不充分.利用多源遥感影像,采用特征追踪方法获取了藏东南则隆弄冰川的表面速度.结合冰川坡度、厚度等地形要素,以及30 a平均气温和降水量等气象数据,分析了其长期流动特征.结果表明,该冰川流速具有显著的季节性:夏秋季较快,春冬季较慢.流速主要受坡度和厚度影响,并在全球变暖背景下呈现缓慢上升趋势.进一步结合气候数据发现,冰川流速变化受季节性气温和降水控制,其中降水的影响存在一定滞后.这种滞后性与降水下渗并传递至冰川底部所需的时间密切相关.长期观测揭示了则隆弄冰川的季节性流动特征和逐渐增强的长期趋势.同时,研究还探讨了流速异常与地质灾害的关系.总体来看,本研究为理解气候变化对藏东南地区冰川动态的影响提供了科学依据.

       

    • 图  1  研究区地理位置及周围部分村落情况

      Fig.  1.  Location of study area and the situation of some surrounding villages

      图  2  研究区现场照片

      Fig.  2.  On-site photos of the Zelongnong glacier

      图  3  则隆弄冰川不同时期流速

      Fig.  3.  The velocity distribution of the Zelongnong glacier at different stages

      图  4  则隆弄冰川年平均流动速度变化

      Fig.  4.  The annual average flow velocity variation of the Zelongnong glacier

      图  5  则隆弄冰川流速季节分布

      Fig.  5.  Seasonal distribution of flow velocity in the Zelongnong glacier

      图  6  则隆弄冰川2022-07~2023-07平均速度分布差异及GNSS测站位置

      Fig.  6.  The velocity distribution differences of the Zelongnong glacier in 2022-07-2023-07 and the location of GNSS monitoring station

      图  7  则隆弄冰川流速计算数据与实测数据对比

      Fig.  7.  A comparison chart of the calculated flow velocity data and the measured data of the Zelongnong glacier

      图  8  则隆弄冰川流速与坡度及冰川厚度对比

      Fig.  8.  A comparison chart of the flow velocity, slope and thickness of the Zelongnong glacier

      图  9  气候变化与对应时间段平均流速的变化关系

      Fig.  9.  The relationship between climate change and the variation of average flow velocity in the corresponding time period

      表  1  遥感数据及冰川数据

      Table  1.   The remote sensing data and glacier data

      数据 时间 来源 数量(张) 分辨率(m) 参考文献及数据库
      冰川运动速度 1994-12~2011-08 Landsat 4-5 TM 117 10 本文
      2010-12~2017-01 Landsat 7 ETM+ 62 30
      2016-11~2024-11 Sentinel-2 L2A 123 30
      数字高程模型 2022 Copernicus 30 30 European Space Agency and Airbus (2022)
      冰川厚度 2017 RGI6.0 RGI Consortium (2017)
      冰川中心线 2023 RGI7.0 RGI Consortium (2023)
      GNSS 2022-7~2023-7 监测仪器 本文
      下载: 导出CSV
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