干旱区研究 ›› 2022, Vol. 39 ›› Issue (2): 638-645.doi: 10.13866/j.azr.2022.02.30
杨维涛1,2,3(),孙建国1,2,3(
),马恒利1,2,3,黄卓1,2,3
收稿日期:
2021-05-18
修回日期:
2021-11-19
出版日期:
2022-03-15
发布日期:
2022-03-30
通讯作者:
孙建国
作者简介:
杨维涛(1994-),男,硕士研究生,主要从事数字地形分析、环境遥感应用研究. E-mail: 基金资助:
YANG Weitao1,2,3(),SUN Jianguo1,2,3(
),MA Hengli1,2,3,HUANG Zhuo1,2,3
Received:
2021-05-18
Revised:
2021-11-19
Online:
2022-03-15
Published:
2022-03-30
Contact:
Jianguo SUN
摘要:
地貌形态对象往往大小悬殊,跨越特定的空间尺度。现有的地貌形态自动分类方法尚未充分顾及该特点,分类精度受到制约。利用地貌形态的大小为尺度,提出1种涉及尺度跨越性的地貌形态多尺度综合分类方法,该方法由多尺度分割、按尺度顺序筛选和多尺度合并3个步骤构成。其中,按尺度顺序筛选是1个以多尺度特征提取和监督分类为基础、以小尺度(小尺寸)优先和概率最大化为准则的被分类对象迭代确认过程。以黄土高原为例的试验结果表明,该方法简便可靠(总体精度可以达到75.16%,Kappa系数可以达到0.71),可用于地貌形态精细化分类。
杨维涛,孙建国,马恒利,黄卓. 地貌形态多尺度综合分类方法[J]. 干旱区研究, 2022, 39(2): 638-645.
YANG Weitao,SUN Jianguo,MA Hengli,HUANG Zhuo. A multi-scale integrated classification method for landforms[J]. Arid Zone Research, 2022, 39(2): 638-645.
表3
地貌形态分级精度评定"
G1 | G2 | G3 | ||||||
---|---|---|---|---|---|---|---|---|
PA/% | UA/% | PA/% | UA/% | PA/% | UA/% | |||
100 | 59.43 | 58 | 70.61 | 75.75 | 80.16 | 87.95 | ||
200 | 58.95 | 65.73 | 71.7 | 77.68 | 75.74 | 73.09 | ||
400 | 61.88 | 71.57 | 77.72 | 75.81 | 72.8 | 75.99 | ||
800 | 65.64 | 65.84 | 75.03 | 81.93 | 60.71 | 68.14 | ||
1200 | 77.45 | 77.19 | 73.5 | 79.57 | 55.81 | 62.9 | ||
2000 | 79.56 | 77.86 | 67.25 | 68.43 | 46.25 | 55.54 | ||
MSIC | 88.89 | 75.27 | 80.33 | 82.77 | 88.29 | 88.39 |
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