基于地理空间方法的高度城市化地区一段时间内土地利用/土地覆盖和地表温度的动态变化

O. Acharya, Dr. Bharat Maitreya
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引用次数: 0

摘要

土地利用/土地覆盖的变化可能对地表温度产生潜在影响。非穿透性土地利用地物可以提高地表温度,而植被覆盖可以降低地表温度。在这项研究中,我们研究了古吉拉特邦索拉斯特拉邦拉杰科特市的土地利用和温度变化。在这里,我们使用了2000年、2010年和2020年地球资源卫星的图像。我们还分析了地表温度,以了解土地利用和土地覆被的变化对城市地表温度的影响。我们发现,在过去的30年里,城市的荒地和休耕地减少了,定居点、湿地、植被覆盖和工业区增加了。随后,人们注意到地表温度的变化。在荒地和休耕地减少的区域,地表温度降低,而在湿地和植被覆盖增加的区域,地表温度升高。在局地尺度上,人类住区和植被覆盖取代荒地和休耕地可以降低地表温度。
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Dynamics of Land-use/Land-cover and Land Surface Temperature over a period of time in a highly urbanized area using a geospatial approach
The changes in land use/land cover can potentially impact the land surface temperature. The land-use features that are impenetrable can increase the Land Surface Temperature, while vegetation cover can decrease the Land Surface Temperature. In this study, we examined the Rajkot city in Saurashtra, Gujarat concerning changes in land use and temperature. Here, we used the imageries from Landsat for the years 2000, 2010, and 2020. We also analyzed the Land Surface Temperature to see how the changes in Land Use Land Cover influence the Land Surface Temperature of the city. We found that across three decades, the city's barren land and fallow land have been decreased and settlement, wetlands, vegetation cover, and industrial areas have been increased. Subsequently, the changes in Land Surface Temperature were noticed. The Land Surface Temperature decreased in the regions where barren land and fallow land are decreased while Land Surface Temperature increased in the areas where wetlands and vegetation cover increased. We conclude that the replacement of the barren and fallow land with human settlement and vegetation cover can decrease the Land Surface Temperature at the local scale.
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发文量
47
审稿时长
16 weeks
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