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中天山典型区域雪崩动力学特征及空间分布

杜帅良 杨金明 黄法融 冯挺 李宏达 杨治纬 魏雯瑜 李兰海

干旱区研究2026,Vol.43Issue(9):1805-1820,16.
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干旱区研究2026,Vol.43Issue(9):1805-1820,16.DOI:10.13866/j.azr.2026.09.02

中天山典型区域雪崩动力学特征及空间分布

Dynamic characteristics of snow avalanches and their spatial patterns in typical regions of the Central Tianshan Mountains

杜帅良 1杨金明 2黄法融 2冯挺 1李宏达 1杨治纬 3魏雯瑜 4李兰海5

作者信息

  • 1. 中国科学院新疆生态与地理研究所,新疆 乌鲁木齐 830011||中国科学院大学,北京 100049
  • 2. 中国科学院新疆生态与地理研究所,新疆 乌鲁木齐 830011
  • 3. 中国科学院新疆生态与地理研究所,新疆 乌鲁木齐 830011||中国科学院大学,北京 100049||新疆交通规划勘察设计研究院有限公司,新疆高寒高海拔山区交通基础设施安全与健康重点实验室,新疆 乌鲁木齐 830006
  • 4. 新疆工程学院土木工程学院,新疆 乌鲁木齐 830023
  • 5. 中国科学院大学,北京 100049||浙江工业大学地理信息学院,浙江 杭州 310023
  • 折叠

摘要

Abstract

Snow avalanches frequently occur in the Central Tianshan Mountains during winter and spring,seri-ously threatening regional transportation,life,and property.However,their dynamic characteristics and spatial distribution remain unclear.Moreover,the evolution of avalanche dynamics across different motion stages and paths remains unclear,hindering scientific hazard assessment.Based on field investigations and remote sensing data,this study examines 76 avalanches that occurred during the mid-winter of a typical year in an avalanche-prone area of the Central Tianshan Mountains.The spatial distribution characteristics of regional snow avalanch-es were analyzed,and their dynamic characteristics and spatiotemporal evolution were investigated using the RAMMS avalanche model.The results indicate the following:(1)Mid-winter avalanches in the study area are pri-marily triggered by continuous snowfall and snowstorms,with drastic diurnal temperature fluctuations acting as the inducing factor.Most avalanches are small in scale(approximately 88%),occur on sunny slopes(89%),and occur on slopes of 25°-50°(88%).(2)Dynamic characteristics differed substantially among different avalanche sites:release volumes ranged from 8.5 to 672.2 m3,maximum flow heights from 0.33 to 2.05 m,maximum flow ve-locities from 2.8 to 15.1 m·s-1,and maximum impact pressures from 1.84 to 68.65 kPa.Runout distance and slope gradient markedly influenced avalanche dynamics.(3)A typical avalanche lasts approximately 130 s.Velocity and impact pressure increase during the initial stage,kinetic energy remains relatively high during sliding,and dynamic forces diminish during deposition.Flow height along the motion path first decreases and increases,whereas impact pressure first increases and decreases,with both trends markedly influenced by terrain convergence.These findings reveal the dynamic characteristics of snow avalanches in typical regions of the Central Tianshan Mountains and pro-vide references for regional avalanche prevention and transportation risk management.

关键词

雪崩/动力学特征/空间分布/RAMMS模型/中天山

Key words

snow avalanche/dynamics characteristics/spatial distribution/RAMMS model/Central Tianshan Mountains

引用本文复制引用

杜帅良,杨金明,黄法融,冯挺,李宏达,杨治纬,魏雯瑜,李兰海..中天山典型区域雪崩动力学特征及空间分布[J].干旱区研究,2026,43(9):1805-1820,16.

基金项目

国家重点研发计划项目(2024YFC3013400) (2024YFC3013400)

第三次新疆综合科学考察项目(2022xjkk0600) (2022xjkk0600)

西藏自治区科技计划项目(XZ202-501ZY0006) (XZ202-501ZY0006)

干旱区研究

1001-4675

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