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国土资源遥感  2018, Vol. 30 Issue (3): 136-142    DOI: 10.6046/gtzyyg.2018.03.19
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空间自相关局部指标在城市热岛界定中的应用
江振蓝1, 龚振彬2, 潘辉3(), 张宝玉1, 王婷芬1
1. 闽江学院地理科学系,福州 350108
2. 福州市气象局, 福州 350008
3. 闽江学院,福州 350108
Application of local spatial autocorrelation indices to the delimitation of urban heat island
Zhenlan JIANG1, Zhenbin GONG2, Hui PAN3(), Baoyu ZHANG1, Tingfen WANG1
1. Department of Geographical Science, Minjiang University, Fuzhou 350108, China
2. Fuzhou Meterorological Service, Fuzhou 350008, China
3. Minjiang University, Fuzhou 350108, China
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摘要 

为探讨空间自相关局部指标在城市热岛界定中的有效性和局限性,运用目前常用的6种算法对福州市Landsat8热红外数据进行地表温度(land surface temperature,LST)反演,利用Moran’s I指数(local Moran’s I index)和G系数(Getis-Ord local G)法界定福州的热岛范围; 比较基于不同LST反演算法的界定结果,并将结果与等间距法、均值标准差法和区域均值分级法进行对比分析。结果表明: Moran’s I指数法和G系数法均能较准确地确定热岛范围,但G系数法界定的热岛范围较Moran’s I指数法更符合实际,对不同LST反演算法的依赖性较小,并与目前常用的热岛界定方法更具可比性,更适合应用于城市热岛界定; G系数法兼顾了LST的高低及其空间相关关系,其界定的城市热岛范围具有明确的统计学意义,而且阈值无需人为干涉,结果更为客观和准确,可在城市热岛定量研究中进一步推广。

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江振蓝
龚振彬
潘辉
张宝玉
王婷芬
关键词 城市热岛热岛界定Moran's I指数;G系数    
Abstract

In this paper, two spatial autocorrelation indices were used to delimit urban heat island in Fuzhou City in a statistical sense. The effectiveness and limitation of the two indices were then analyzed so as to find effective methods for quantitative study of urban heat island. At first, land surface temperature (LST) was retrieved on the basis of Landsat8 thermal infrared data of Fuzhou City by applying 6 methods that are frequently used. Then Local Moran’s I Index and Getis-Ord local G were used to delimit urban heat island in the study area. At last the different delimitation outcomes were compared with each other and were then compared with the outcomes obtained by other methods, including equal interval method, mean standard deviation method and regional average classification method. The findings are as follows: ① Both Local Moran’s I index and Getis-Ord local G accurately delimit urban heat island. By comparison, Getis-Ord local G is more accurate in heat island delimitation and is less dependent on methods of LST retrieval. It is more comparable with other heat island delimitation methods; ② The method applying Getis-Ord local G takes into account both surface temperature and spatial correlation of temperature, which makes the delimitation outcome statistically meaningful. With its threshold value free of human factors, the method is therefore more objective and more applicable in the quantitative study of urban heat island.

Key wordsurban heat island    delimitation of urban heat island    local Moran's I index;    Getis-Ord local G
收稿日期: 2017-02-08      出版日期: 2018-09-10
:  TP79  
基金资助:国家自然科学基金项目“基于农用地养分收支平衡的多情景畜禽粪便还田空间分配研究”(41601601);福建省自然基金项目“格网尺度土壤重金属的高光谱遥感预测——以重金属Cr为例”(2016J01194);福州市科技计划项目“福州城市热环境时空分异与区别”(2017S136);“福州市城市热岛的时空特征及其成因分析”(2014S130);福建省自然基金项目“基于高光谱特征与目标分割的城市地物识别研究”(2015J01627)
通讯作者: 潘辉
作者简介: 江振蓝(1977-),女,博士,副教授,主要从事生态环境遥感研究。Email: jessie33cn@163.com。
引用本文:   
江振蓝, 龚振彬, 潘辉, 张宝玉, 王婷芬. 空间自相关局部指标在城市热岛界定中的应用[J]. 国土资源遥感, 2018, 30(3): 136-142.
Zhenlan JIANG, Zhenbin GONG, Hui PAN, Baoyu ZHANG, Tingfen WANG. Application of local spatial autocorrelation indices to the delimitation of urban heat island. Remote Sensing for Land & Resources, 2018, 30(3): 136-142.
链接本文:  
https://www.gtzyyg.com/CN/10.6046/gtzyyg.2018.03.19      或      https://www.gtzyyg.com/CN/Y2018/V30/I3/136
Fig.1  研究区LST的空间分布
反演算法 最小值 最大值 平均值 温差 标准差
IB 27.35 44.84 33.44 17.49 3.45
IMW 26.55 58.70 37.04 32.15 6.07
RTE 32.94 62.02 42.69 29.08 5.53
SC 33.15 63.89 43.33 30.74 5.82
SW_JM 27.54 54.84 36.35 27.30 5.11
SW_R 29.61 55.46 38.34 25.85 4.87
Tab.1  基于不同算法反演的LST统计特征
Fig.2  利用Moran’s I指数法和G系数法提取的城市热场空间分布图
反演算法 Morans’I指数法 G系数法
热岛区 冷岛区 常温区 热岛区 冷岛区 常温区
IB 25.41 22.76 51.83 28.65 26.69 44.66
IMW 25.10 24.38 50.52 28.36 27.91 43.73
RTE 25.25 24.25 50.50 28.48 27.80 43.72
SC 25.17 24.37 50.46 28.40 27.85 43.75
SW_JM 25.69 24.95 49.36 29.03 28.74 42.23
SW_R 25.60 25.95 48.25 29.23 29.53 41.24
Tab.2  城市热场信息提取统计
Fig.3  Moran’s I指数法与G系数法对LST反演算法的敏感性
Fig.4  空间自相关局部指标法与常规城市热岛界定方法的可比性
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