在吉拉丹东地区的冰川边界提取和时空变化分析
Haotian Liu1, Dongchuan Wang1,2, Tingrong Li1
1School of Geology and Geomatics, Tianjin Chengjian University, Tianjin, China.
PeerJ
|February 23, 2026
概括
由于气候变化,冰川正在缩小,在2010-2015年期间观察到显著的撤退. 一种新的NDI-RF方法准确地绘制了冰川范围,性能优于现有技术.
科学领域:
- 冰川学的冰川学
- 气候科学 气候科学
- 遥感 遥感 遥感 遥感
背景情况:
- 冰川是全球气候变化的关键指标,影响水循环和海平面.
- 了解冰川动态需要分析气候,地形和边界变化之间的相互作用.
研究的目的:
- 开发和验证一种用于绘制冰川范围的新方法.
- 分析冰川地区的时空变化及其与气候因素的关系.
主要方法:
- 提出了用于冰川绘图的远程传感指数-随机森林 (NDI-RF) 融合方法.
- 根据标准化差异雪指数 (NDSI) 和随机森林模型验证的NDI-RF.
- 分析了从2000年到2024年在吉拉丹东地区的冰川变化.
主要成果:
- 在NDI-RF方法实现了高精度 (卡帕:0.92,OA:0.94,F1:0.92).
- 吉拉丹东地区的冰川在2000年至2024年期间减少了110.29平方公里,从2010年至2015年加速撤退.
- 在5250米以下,在45°以上的斜坡和面向北北的斜坡上,撤退更为明显.
结论:
- 该NDI-RF方法有效地绘制冰川范围,减少光谱混乱.
- 冰川面积与年平均气温上升有负相关性.
- 这些发现凸显了冰川对气候变化和地形因素的敏感性.
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