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基于决策树的高山区堰塞湖水体提取方法: 以中巴公路Attabad堰塞湖为例

李有三 曹广超 赵美亮 冶文倩 祁万强 杨鸿魁 毋远召 谷强 陆裕国 王仕林

李有三, 曹广超, 赵美亮, 冶文倩, 祁万强, 杨鸿魁, 毋远召, 谷强, 陆裕国, 王仕林. 基于决策树的高山区堰塞湖水体提取方法: 以中巴公路Attabad堰塞湖为例[J]. 地质科技通报, 2024, 43(6): 51-62. doi: 10.19509/j.cnki.dzkq.tb20240125
引用本文: 李有三, 曹广超, 赵美亮, 冶文倩, 祁万强, 杨鸿魁, 毋远召, 谷强, 陆裕国, 王仕林. 基于决策树的高山区堰塞湖水体提取方法: 以中巴公路Attabad堰塞湖为例[J]. 地质科技通报, 2024, 43(6): 51-62. doi: 10.19509/j.cnki.dzkq.tb20240125
LI Yousan, CAO Guangchao, ZHAO Meiliang, YE Wenqian, QI Wanqiang, YANG Hongkui, WU Yuanzhao, GU Qiang, LU Yuguo, WANG Shilin. A method for extracting water from barrier lake in high mountain areas based on decision tree classification: A case study of Attabad barrier lake on the Karakoram Highway[J]. Bulletin of Geological Science and Technology, 2024, 43(6): 51-62. doi: 10.19509/j.cnki.dzkq.tb20240125
Citation: LI Yousan, CAO Guangchao, ZHAO Meiliang, YE Wenqian, QI Wanqiang, YANG Hongkui, WU Yuanzhao, GU Qiang, LU Yuguo, WANG Shilin. A method for extracting water from barrier lake in high mountain areas based on decision tree classification: A case study of Attabad barrier lake on the Karakoram Highway[J]. Bulletin of Geological Science and Technology, 2024, 43(6): 51-62. doi: 10.19509/j.cnki.dzkq.tb20240125

基于决策树的高山区堰塞湖水体提取方法: 以中巴公路Attabad堰塞湖为例

doi: 10.19509/j.cnki.dzkq.tb20240125
基金项目: 

青海省创新平台建设专项 2020-ZJ-Y06

中国地质调查局地质调查项目 DD20242544

详细信息
    作者简介:

    李有三, E-mail: liyousan@mail.cgs.gov.cn

    通讯作者:

    曹广超, E-mail: caoguangchao@qhnu.edu.cn

  • 中图分类号: P237;P343.3

A method for extracting water from barrier lake in high mountain areas based on decision tree classification: A case study of Attabad barrier lake on the Karakoram Highway

More Information
  • 摘要:

    堰塞湖水体动态监测对于堰塞湖的险情评估、灾害推演、安全管理以及降险处置决策等均具有重要意义。为了高效提取高山区堰塞湖真实水体范围, 以中巴公路Attabad堰塞湖为研究区, 利用决策树分类结合归一化差值水体指数(normalized difference water index, 简称NDWI)、综合水体指数(comprehensive water index, 简称CWI)等6种常规水体提取方法来提取堰塞湖水体范围, 并对比了6种方法用于堰塞湖水体提取的效果, 筛选出适用于高山区堰塞湖的最佳水体提取方法, 最后使用混淆矩阵法进行了精度评价, 并做了分类后处理, 准确提取了堰塞湖水体边界。研究结果表明: (1) 6种水体提取模型中CWI模型水体提取效果最好; (2)基于坡度的决策树分类方法总分类精度为89.31%, Kappa系数为0.84, 较为完整地提取了高海拔堰塞湖真实水体范围, 有效剔除了湖岸斜坡山体阴影, 湖泊边界较为清晰完整。基于决策树的高山区堰塞湖水体提取方法在高海拔山区能较为有效地提取真实水体范围, 尤其是针对地形切割强烈、山体阴影较多的堰塞湖区域, 能快速准确识别水体。该方法的优点是: 水体提取过程较为简单, 容易实现, 提取效率较高, 便于推广。

     

  • 图 1  Attabad堰塞湖位置图

    Figure 1.  Location map of Attabad barrier lake

    图 2  研究流程图

    B4、NDWI、ENDWI、CWI、C3/NIR、SI均表示水体提取方法,其中B4表示单波段B4阈值法,NDWI表示归一化差值水体指数法,CWI表示综合水体指数法,ENDWI表示改进的归一化水体指数法,C3/NIR表示彩色不变特征空间法,SI表示阴影指数法,下同

    Figure 2.  Research flow chart

    图 3  波谱特征曲线图(DN为地物的灰度值)

    Figure 3.  Spectrum characteristic curve

    图 4  决策树模型

    Figure 4.  Decision tree model

    图 5  各水体提取模型值域箱线图(其中SL表示斜坡;W表示水体;WS表示阴影水体)

    Figure 5.  Value range box diagram of each water extraction model

    图 6  各水体提取模型水体提取分类图

    Figure 6.  Extraction and classification of water bodies in each water extraction model

    图 7  基于决策树模型与CWI模型图像对比

    Figure 7.  Comparison of images based on decision tree classification and CWI models

    表  1  应用于高分辨率影像的6种水体提取模型

    Table  1.   Six water extraction models applied to high-resolution images

    模型 方程 特征
    B4 b4>R R为根据研究区水体信息判断的经验阈值,特点是操作简单,便于实现
    NDWI $N D W I=\left(b_2-b_4\right) /\left(b_2+b_4\right)$ 有效抑制非水体,但难以区分土壤和阴影
    ENDWI $\mathit{ENDWI}=\left(b_2-b_4\right) /\left(2 b_2\right)$ 增强水体与冰雪、阴影的反差,减少背景噪音
    CWI $C W I=3 b_4-b_2-b_1$ 抑制阴影
    C3/NIR $C_3=\tan ^{-1}\left(b_1 / \max \left(b_3, b_2\right)\right), C_3 / b_4$ 提取阴影,突出阴影中的水体
    SI $S I=\left(F C_3-P C I_1\right) /\left(F C_3+P C I_1\right)$ PCI1为主成分变换后的第一分量;F为补偿系数,根据C3PCI1的值域经验判断得出F=1 000较为合适。特点是能突出阴影,增强水体信息
    注:NDWI表示归一化差值水体指数;CWI表示综合水体指数;ENDWI表示改进的归一化水体指数;SI表示阴影指数法;b1代表蓝波段;b2代表绿波段;b3代表红波段;b4代表近红外波段;C3代表彩色不变特征空间方法中的C3分量; 下同
    下载: 导出CSV

    表  2  分类精度

    Table  2.   Classification accuracy

    分类类别 总计 用户精度/%
    斜坡 阴影水体 水体
    分类类别 斜坡 52 16 0 68 74.47
    阴影水体 0 34 0 34 100.00
    水体 0 1 56 57 98.25
    总计 52 51 56 159
    制图精度/% 100 66.67 100
    注:总体精度为89.31%,Kappa系数为0.84
    下载: 导出CSV
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出版历程
  • 收稿日期:  2024-03-28
  • 录用日期:  2024-07-01
  • 修回日期:  2024-05-30

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