Mitigation of urban heat island in China (2000–2020) through vegetation-induced cooling

被引:0
|
作者
Wu B. [1 ,2 ]
Zhang Y. [3 ]
Wang Y. [1 ,2 ]
He Y. [4 ]
Wang J. [5 ]
Wu Y. [5 ]
Lin X. [6 ]
Wu S. [1 ,2 ]
机构
[1] Key Laboratory of Humid Subtropical Eco-geographical Processes of Ministry of Education, School of Geographical Sciences, Fujian Normal University, Fuzhou
[2] Institute of Geography, Fujian Normal University, Fuzhou
[3] Jiangsu Provincial Key Laboratory of Geographic Information Science and Technology, International Institute for Earth System Science, Nanjing University, Nanjing
[4] Faculty of Economics, Otemon Gakuin University, Osaka
[5] School of Culture Tourism and Public Administration, Fujian Normal University, Fuzhou
[6] School of Sociology and History, Fujian Normal University, Fuzhou
基金
中国国家自然科学基金;
关键词
City afforestation; Surface temperature variations; Urban and non-urban areas; Urban heat island effect; Vegetation cooling benefits;
D O I
10.1016/j.scs.2024.105599
中图分类号
学科分类号
摘要
City afforestation serves as a robust strategy for thermal mitigation. Employing multisource satellite data, we explored the impact of vegetation cover on temperature dynamics across urban and rural sectors in Chinese cities. Our analysis reveals that a 1 % increase in vegetation coverage corresponds to a reduction in surface temperature by 0.099 °C to 0.102 °C in urban environments. However, the cooling effect diminishes from urban to rural areas, where increased vegetation occasionally results in warming. Further, the temperature reduction tends to stabilize at higher vegetation levels, as demonstrated in grid-based evaluations. Significantly, variations in urban population density substantially modulate these cooling effects. Over the period 2000–2020, afforestation increased vegetation coverage by 4.35 % in urban areas, which led to cooling in 67.43 % of the analyzed cities, with an average surface temperature decline of 0.58 °C. Additionally, our findings document a notable attenuation of the urban heat island (UHI) effect over time, with an average decrease of 0.56 ± 0.35 °C. This reduction primarily results from the thermoregulatory effects of changes in vegetation coverage, which cool urban areas and may warm rural ones. Our study underscores the critical role of afforestation in urban climate management and its efficacy in attenuating urban heat waves and UHI effects. © 2024 Elsevier Ltd
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