Spatio-Temporal Analysis of Surface Urban Heat Island and Canopy Layer Heat Island in Beijing

• Published in: Applied sciences Vol. 14; no. 12; p. 5034
• Main Authors: Yuan, Debao, Zhang, Liuya, Fan, Yuqing, Sun, Wenbin, Fan, Deqin, Zhao, Xurui
• Format: Journal Article
• Language: English
• Published: Basel MDPI AG 01.06.2024
• Subjects: canopy layer heat island; Economic development; Gaussian volume model; Remote sensing; Suburban areas; Summer; surface urban heat island; Urban climatology; Urban development; Urban health; urban heat island effect; Urban heat islands; Vegetation; Winter; Beijing China; China
• ISSN: 2076-3417; 2076-3417
• DOI: 10.3390/app14125034

Studying urban heat islands holds significance for the sustainable development of cities. This comprehensive study analyzed the temporal characteristics of a Surface Urban Heat Island and Canopy Layer Heat Island by employing Moderate-Resolution Imaging Spectroradiometer image data spanning from 2003 to 2020 over Beijing, China. Leveraging the Gaussian capacity model, the geometrical characteristics of the Surface Urban Heat Island and Canopy Layer Heat Island, such as intensity, center, direction, and range, were examined among three different timescales of day, month, and year. Results indicate that the intensities of the Surface Urban Heat Island and Canopy Layer Heat Island tend to have bigger seasonal variations during winter nights and summer daytime. In addition, at night the centers of Surface Urban Heat Island and Canopy Layer Heat Island are mainly concentrated in the range of 116.3°~116.4° E in longitude and 39.90°~39.95° N in latitude, while during the daytime they are more scattered, mainly in the range of 116.2°~116.5° E in longitude and 39.7°~40.0° N in latitude. In the hot season, the center of the heat island moves east to north, while in the cold season it moves west to south. Monthly average ellipse areas of Surface Urban Heat Island and Canopy Layer Heat Island vary more during the day than that at night, the maximum daytime differences were 2662 km[sup.2] and 2293 km[sup.2], while the maximum nighttime differences were 484 km[sup.2] and 265 km[sup.2]. Overall, the average area is increasing, with the heat island center moving eastward and deflecting towards the northeast-southwest direction. The expansion of urban areas will continue to influence the movement and extent of heat islands. The study offers insights to inform strategies for mitigating urban heat islands.