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利用 Landsat 卫星图像和 Ndaisi 方法数据增强,研究半干旱地区不透水面、植被和土壤对地表温度的影响。

The impact of impervious surface, vegetation, and soil areas on land surface temperatures in a semi-arid region using Landsat satellite images enriched with Ndaisi method data.

机构信息

Department of Geomatics Engineering, Usak University, Usak, Turkey.

Department of Geomatics Engineering, Erciyes University, Kayseri, Turkey.

出版信息

Environ Monit Assess. 2021 Feb 24;193(3):143. doi: 10.1007/s10661-021-08916-3.

DOI:10.1007/s10661-021-08916-3
PMID:33625580
Abstract

Impervious surfaces are a significant issue of both urbanization and environmental assessment. However, it is a problem to classify impervious surface (IS) and soil areas as separate classes in land cover classification. The objectives of this study are to obtain impervious surface, vegetation, and soil areas clearly of an urban complex with a semi-arid climate and to better determine the relationships of IS, vegetation, and soil areas with land surface temperatures (LSTs). For this purpose, IS, vegetation, and soil areas in a semi-arid city of Turkey-Kayseri city were identified by using Normalized Difference Anthropogenic Impervious Surface Index (NDAISI) data and support vector machine (SVM) method together in the classification of different areas. Landsat 5, 7, and 8 satellite images of 1987, 2000, and 2013 were used, respectively, in this study. Afterward, the effects of these areas on LSTs were analyzed. Regression analysis was used to determine the relationships between land cover areas and surface temperatures. To better demonstrate these relationships, besides common pixel-based and classical regional-based approaches, a new density-based regional analysis approach was proposed. This study is an innovative one in terms of detecting IS and indicating relationships between land cover areas and surface temperatures in semi-arid regions. Another innovation of the study is related to the results produced. The results showed that decreasing LST values were observed with increasing IS and vegetation cover values and increasing LST values were observed with increasing soil areas. The present findings may provide significant contributions to the literature and will facilitate the development of urban planning strategies in semi-arid regions.

摘要

不透水面是城市化和环境评估的一个重要问题。然而,在土地覆盖分类中将不透水面 (IS) 和土壤区域划分为单独的类别是一个问题。本研究的目的是明确获得具有半干旱气候的城市综合体的不透水面、植被和土壤区域,并更好地确定 IS、植被和土壤区域与地表温度 (LST) 的关系。为此,使用归一化差异人工不透水面指数 (NDAISI) 数据和支持向量机 (SVM) 方法在分类中一起识别了土耳其半干旱城市-开塞利市的不透水面、植被和土壤区域。本研究分别使用了 1987 年、2000 年和 2013 年的 Landsat 5、7 和 8 卫星图像。之后,分析了这些区域对 LST 的影响。回归分析用于确定土地覆盖区域与地表温度之间的关系。为了更好地展示这些关系,除了常见的基于像素和经典的基于区域的方法外,还提出了一种新的基于密度的区域分析方法。就检测 IS 并指示半干旱地区土地覆盖区域与地表温度之间的关系而言,本研究具有创新性。研究的另一个创新点与产生的结果有关。结果表明,随着 IS 和植被覆盖值的增加,LST 值降低,随着土壤面积的增加,LST 值增加。本研究结果可能对文献有重要贡献,并将有助于半干旱地区城市规划策略的制定。

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