4.7 Article

Spatial configuration and time of day impact the magnitude of urban tree canopy cooling

期刊

ENVIRONMENTAL RESEARCH LETTERS
卷 16, 期 8, 页码 -

出版社

IOP Publishing Ltd
DOI: 10.1088/1748-9326/ac12f2

关键词

urban heat island; urban forest; air temperature; landscape context; tree canopy

资金

  1. National Science Foundation [1951647]
  2. Direct For Social, Behav & Economic Scie
  3. Division Of Behavioral and Cognitive Sci [1951647] Funding Source: National Science Foundation

向作者/读者索取更多资源

The study shows that trees can lower air temperatures in urban environments. The cooling effects of hard and soft canopies vary at different times of day, with soft canopies showing the most significant cooling effect in the evening. Distributed canopies have better cooling effects in predawn and evening, which is crucial for urban heat island mitigation planning.
Tree cover is generally associated with cooler air temperatures in urban environments but the roles of canopy configuration, spatial context, and time of day are not well understood. The ability to examine spatiotemporal relationships between trees and urban climate has been hindered by lack of appropriate air temperature data and, perhaps, by overreliance on a single 'tree canopy' class, obscuring the mechanisms by which canopy cools. Here, we use >70 000 air temperature measurements collected by car throughout Washington, DC, USA in predawn (pd), afternoon (aft), and evening (eve) campaigns on a hot summer day. We subdivided tree canopy into 'soft' (over unpaved surfaces) and 'hard' (over paved surfaces) canopy classes and further partitioned soft canopy into distributed (narrow edges) and clumped patches (edges with interior cores). At each level of subdivision, we predicted air temperature anomalies using generalized additive models for each time of day. We found that the all-inclusive 'tree canopy' class cooled linearly at every time (pd = 0.5 degrees C +/- 0.3 degrees C, aft = 1.8 degrees C +/- 0.6 degrees C, eve = 1.7 degrees C +/- 0.4 degrees C), but could be explained in the afternoon by aggregate effects of predominant hard and soft canopy cooling at low and high canopy cover, respectively. Soft canopy cooled nonlinearly in the afternoon with minimal effect until similar to 40% cover but strongly (and linearly) across all cover fractions in the evening (pd = 0.7 degrees C +/- 1.1 degrees C, aft = 2.0 degrees C +/- 0.7 degrees C, eve = 2.9 degrees C +/- 0.6 degrees C). Patches cooled at all times of day despite uneven allocation throughout the city, whereas more distributed canopy cooled in predawn and evening due to increased shading. This later finding is important for urban heat island mitigation planning since it is easier to find planting spaces for distributed trees rather than forest patches.

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