School of Architecture, Tsinghua University, Beijing, 100084, China.
Department of City and Regional Planning, The Ohio State University, 275 West Woodruff Avenue, Columbus, OH, 43210, USA.
J Environ Manage. 2022 Dec 15;324:116263. doi: 10.1016/j.jenvman.2022.116263. Epub 2022 Sep 24.
As most cities are located around or near waterbodies, it is essential to assess the thermal effect of these waterbodies. This research focuses on 34 Chinese megacities as case studies to examine the spatial relationship between city-water layout and the thermal effect of waterbodies. Landsat-8 remote-sensing images acquired around noontime in summer were used to retrieve land surface temperatures (LST) and classify land cover. The results show that there are three types of city-water layout. For most cities, waterbodies have a cooling effect, and their mean cooling distance (ΔL) ranges from 431 m to 1350 m, with the maximum temperature difference (ΔT) ranging from - 2.21 °C to 7.83 °C. The cooling effect of waterbodies is also influenced by their spatial distribution, size, location, and background climate regions. The larger the percentage or area of waterbodies in a city, the shorter ΔL and the bigger ΔT. Waterbodies have the longest ΔL and the smallest ΔT when they are dispersed within the city, whereas they have the shortest ΔL and the largest ΔT when they are flowing through the city. The results suggest that the thermal effects of waterbodies should be seriously considered by urban planners to improve the urban microclimate.
由于大多数城市都位于水体周围或附近,因此评估这些水体的热效应至关重要。本研究以 34 个中国特大城市为案例研究,考察了城市-水体布局与水体热效应之间的空间关系。利用夏季正午时分获取的 Landsat-8 遥感图像来反演地表温度(LST)并进行土地覆盖分类。结果表明,城市-水体布局有三种类型。对于大多数城市而言,水体具有冷却效应,其平均冷却距离(ΔL)范围为 431 米至 1350 米,最大温差(ΔT)范围为-2.21°C 至 7.83°C。水体的冷却效应还受到其空间分布、大小、位置和背景气候区域的影响。城市中水体的百分比或面积越大,ΔL 越短,ΔT 越大。当水体在城市内部分散分布时,ΔL 最长,ΔT 最小;而当水体流经城市时,ΔL 最短,ΔT 最大。研究结果表明,城市规划者应认真考虑水体的热效应,以改善城市微气候。