Understanding urban atmospheric variability: Implications of vegetation (canopy cover) dynamics in Assam's urban landscapes

IF 5.4 Q1 ENVIRONMENTAL SCIENCES
Rupjyoti Nath , Sujit Deka
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引用次数: 0

Abstract

Large-scale urbanization has altered city surface characteristics, significantly affecting heat balance and thermal environments. The role of vegetative and urban canopy cover in shaping metropolitan climates has gained considerable attention.This study examines the impact of tree canopy cover on thermal comfort and microclimatic conditions in Guwahati, Assam. Conducted in a high-temperature, high-humidity region, it uses qualitative surveys and microclimatic measurements, alongside remote sensing data from 1981 to 2022. Findings show that without canopy cover, car roof temperatures reach 26.32 °C, while areas with high canopy coverage have lower temperatures of 21.17 °C. Vegetation analysis reveals a 10.06% decline in canopy cover, a 13.46% increase in built-up areas, and a 3.85% decrease in open spaces. A negative correlation between NDVI and LST confirms that reduced vegetation increases surface temperatures.The study confirms a negative correlation between NDVI and LST, with coefficients ranging from −.468 to −.224, showing that reduced vegetation increases surface temperatures. Areas with high tree canopy cover experience significant microclimate benefits, with afternoon air and mean radiant temperatures lowered by up to 4.9 °C and 5.48 °C, respectively. Stations with more canopy cover provide greater cooling effects, especially at noon, compared to areas without tree shade.Increasing tree canopy coverage enhances thermal comfort and supports sustainable urban planning. This study offers valuable insights for managing thermal environments and guiding urban policy and sustainable development.
了解城市大气变异性:阿萨姆邦城市景观中植被(树冠覆盖)动态的影响
大规模城市化改变了城市地表特征,对热平衡和热环境产生了重大影响。本研究探讨了树冠覆盖对阿萨姆邦古瓦哈提的热舒适度和微气候条件的影响。这项研究在高温高湿地区进行,使用了定性调查和微气候测量数据,以及 1981 年至 2022 年的遥感数据。研究结果表明,在没有树冠覆盖的情况下,车顶温度高达 26.32 °C,而树冠覆盖率高的地区温度较低,为 21.17 °C。植被分析显示,树冠覆盖率下降了 10.06%,建筑密集区增加了 13.46%,空地减少了 3.85%。NDVI 和 LST 之间的负相关关系证实,植被减少会增加地表温度。研究证实,NDVI 和 LST 之间存在负相关关系,系数在 -.468 到 -.224 之间,表明植被减少会增加地表温度。树冠覆盖率高的地区具有显著的小气候优势,午后空气温度和平均辐射温度分别降低了 4.9 ℃ 和 5.48 ℃。与没有树荫的地区相比,树冠覆盖率高的站点降温效果更好,尤其是在中午。这项研究为管理热环境、指导城市政策和可持续发展提供了宝贵的见解。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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来源期刊
Environmental and Sustainability Indicators
Environmental and Sustainability Indicators Environmental Science-Environmental Science (miscellaneous)
CiteScore
7.80
自引率
2.30%
发文量
49
审稿时长
57 days
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