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Оценка многопериодного баланса массы ледников западного участка Цилиньшань на основе двойной станционной InSAR и DEM WorldView

  • role： First author第一作者
  • Affiliation：

    State Key Laboratory of Geodesy and Earth’s Dynamics, Innovation Academy for Precision Measurement Science and Technology, Chinese Academy of Sciences, Wuhan 430071, China

    School of Earth and Planetary, University of Chinese Academy of Sciences, Beijing 100049, China

  • Email：ch10lichao@163.com
  • Introduction：李超，研究方向为冰川物质平衡大地测量研究。E-mail：ch10lichao@163.com
LI Chao12,  
  • role： Corresponding author通信作者
  • Affiliation：

    State Key Laboratory of Geodesy and Earth’s Dynamics, Innovation Academy for Precision Measurement Science and Technology, Chinese Academy of Sciences, Wuhan 430071, China

    School of Earth and Planetary, University of Chinese Academy of Sciences, Beijing 100049, China

  • Email：jlm@apm.ac.cn
  • Introduction：江利明，研究方向为影像大地测量理论、方法及应用。E-mail：jlm@apm.ac.cn
JIANG Liming12*,  
  • Affiliation：

    State Key Laboratory of Geodesy and Earth’s Dynamics, Innovation Academy for Precision Measurement Science and Technology, Chinese Academy of Sciences, Wuhan 430071, China

    MOE Key Laboratory of Fundamental Physical Quantities Measurement, School of Physics, Huazhong University of Science and Technology, Wuhan 430074, China

LIU Lin13,  
  • Affiliation：

    State Key Laboratory of Geodesy and Earth’s Dynamics, Innovation Academy for Precision Measurement Science and Technology, Chinese Academy of Sciences, Wuhan 430071, China

    School of Earth and Planetary, University of Chinese Academy of Sciences, Beijing 100049, China

LI Tao12,  
  • Affiliation：

    State Key Laboratory of Geodesy and Earth’s Dynamics, Innovation Academy for Precision Measurement Science and Technology, Chinese Academy of Sciences, Wuhan 430071, China

    School of Geography and Information Engineering, China University of Geosciences, Wuhan 430074, China

CHEN Yuanyuan14

реферат

Баланс массы ледников как чувствительный индикатор изменения климата имеет важное значение для управления региональными водными ресурсами, предотвращения ледниковых катастроф и прогнозирования глобальных изменений уровня моря. С усилением глобального потепления с 2000 года в западной части хребта Цилиньшань ускорилось таяние ледников, однако в последние годы изменения годичного баланса массы ледников, особенно 12-го ледника в долине Лаохугоу, остаются малоизученными. В данной статье с использованием многоданных DEM, полученных методом оптической стереофотограмметрии WorldView, SRTM и двойной станционной InSAR TanDEM-X, применён метод разности DEM для определения скоростей межгодового изменения толщины льда на западном участке Цилиньшань в период 2013–2014, 2014–2015 годов и средней скорости изменения толщины льда за 2000–2015 годы, а также получены соответствующие результаты баланса массы ледников за указанные периоды. На основе этого, на примере 12-го ледника в долине Лаохугоу, оценены скорости изменения баланса массы ледника за периоды 2013–2014, 2014–2015 и 2000–2015 годов, а также проанализировано влияние изменений осадков и температуры на изменение баланса массы. Результаты показали: скорости изменения толщины льда в западной части Цилиньшань в 2013–2014 и 2014–2015 годах составляли -0,35±0,034 м и -0,028±0,004 м соответственно, скорости изменения баланса массы составили -0,27±0,014 м вод. экв./год и -0,024±0,084 м вод. экв./год соответственно. За период 2000–2015 средний баланс массы 12-го ледника в долине Лаохугоу равнялся -0,013±0,02 м вод. экв./год, ледник находился в состоянии таяния. Скорость потерь льда снижалась с -0,33±0,04 м вод. экв./год в 2013–2014 годах до -0,036±0,09 м вод. экв./год в 2014–2015 годах, что в основном связано с увеличением осадков в 2015 году. В статье подтверждена возможность использования высококачественных данных DEM спутниковой оптической стереофотограмметрии для расчёта межгодового баланса массы горных ледников.

ключеви́че слова́

дистанционное зондирование; DEM WorldView; DEM TanDEM-X; ледник номер 12 в долине Лаохугоу; баланс массы; InSAR; Цилиньшань

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