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Remote Sensing for Land & Resources    2019, Vol. 31 Issue (1) : 95-100     DOI: 10.6046/gtzyyg.2019.01.13
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A study of selection method of NDWI segmentation threshold for GF-1 image
Yilin JIA, Wen ZHANG, Lingkui MENG()
College of Remote Sensing Information Engineering, Wuhan University, Wuhan 430079, China
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Abstract  

Based on 15 lakes located in different regions of China, the authors calculated the normalized difference water index (NDWI) for GF-1 satellite remote sensing images, and then employed iterative method, Otsu method and histogram bimodal method for segmentation threshold selection and water information extraction, and finally analyzed the threshold selection results and water information extraction results of the three methods. According to the results obtained, iterative method is similar to the threshold chosen by Otsu method, and the difference between the thresholds selected by histogram bimodal method is large; the iterative method is more efficient; the extraction accuracy of bimodal method is the highest, and its fitting effect is the best. This study can provide selection strategies of adaptive threshold segmentation method for extracting accurate water information from GF-1 images.

Keywords GF-1 data      NDWI      adaptive threshold      water extraction     
:  TP79  
Corresponding Authors: Lingkui MENG     E-mail: Lkmeng@whu.edu.cn
Issue Date: 15 March 2019
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Yilin JIA
Wen ZHANG
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Yilin JIA,Wen ZHANG,Lingkui MENG. A study of selection method of NDWI segmentation threshold for GF-1 image[J]. Remote Sensing for Land & Resources, 2019, 31(1): 95-100.
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https://www.gtzyyg.com/EN/10.6046/gtzyyg.2019.01.13     OR     https://www.gtzyyg.com/EN/Y2019/V31/I1/95
湖区 实验湖泊
东北平原与山地湖区 查干湖
东部平原湖区 洪泽湖、太湖、鄱阳湖、洞庭湖
蒙新湖区 呼伦湖、乌梁素海、乌伦古湖、艾比湖、博斯腾湖
云贵高原湖区 滇池
青藏高原湖区 青海湖、色林错、纳木错、玛旁雍错
Tab.1  Distribution of test lakes
湖泊 影像获取日期 迭代法 大津法 双峰法 湖泊类型
青海湖 20161003 983 967 938 咸水湖
纳木错 20161215 1 168 1 237 1 135 咸水湖
色林错 20161208 1 189 1 222 1 021 咸水湖
艾比湖 20160828 1 217 1 238 1 186 咸水湖
太湖 20161128 951 943 996 淡水湖
滇池 20161114 822 800 859 淡水湖
鄱阳湖 20161104 839 837 918 淡水湖
洞庭湖 20160725 849 824 813 淡水湖
洪泽湖 20160511 885 864 952 淡水湖
乌梁素海 20160992 934 920 1 114 淡水湖
查干湖 20160920 919 925 1 084 淡水湖
博斯腾湖 20160909 967 960 1 038 淡水湖
呼伦湖 20160410 1 021 920 986 淡水湖
玛旁雍错 20161111 1 076 1 062 920 淡水湖
乌伦古湖 20160881 1 092 1 065 1 002 淡水湖
Tab.2  Thresholds of lake images obtained by different methods
Fig.1  Relationship between the image thresholds of lakes obtained by different methods
方法 最小用时 最大用时 平均用时
迭代法 0.046 0.063 0.052
大津法 12.752 14.003 13.223
双峰法 7.500 8.174 7.878
Tab.3  Time of different methods in threshold selection process(s)
地貌
类型
迭代法 大津法 双峰法 总计
水体 非水体 水体 非水体 水体 非水体
水体 654 53 654 53 636 71 707
8 16 7 17 23 1 24
滩涂 42 69 43 68 31 80 111
建筑 31 58 33 56 14 75 89
25 4 25 4 7 22 29
其他 40 500 46 494 36 504 540
Tab.4  Confusion matrix of results extracted by different methods
指标 迭代法 大津法 双峰法
误提率 17.95 19.12 11.44
漏提率 9.44 9.58 9.85
正确率 86.20 85.53 89.33
Tab.5  Extracting precision of different methods(%)
方法 最大值 最小值 总差值 平均值 标准差
迭代法 244.70 0.61 544.23 36.28 65.96
大津法 224.97 0.85 542.63 36.18 62.67
双峰法 190.58 0.23 353.24 23.55 47.62
Tab.6  Statistics of absolute differences between areas extracted by different methods and reference areas(km2)
Fig.2  Relationship between areas extracted by different methods and reference areas
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