Urban tree cover provides consistent mitigation of extreme heat in arid but not humid cities

被引:7
|
作者
Ibsen, Peter C. [1 ]
Crawford, Benjamin R. [2 ]
Corro, Lucila M. [1 ]
Bagstad, Kenneth J. [1 ]
Mcnellis, Brandon E. [3 ]
Jenerette, George D. [4 ]
Diffendorfer, Jay E. [1 ]
机构
[1] US Geol Survey, Geosci & Environm Change Sci Ctr, Lakewood, CO 80225 USA
[2] Univ Colorado Denver, Dept Geog & Environm Sci, Denver, CO 80204 USA
[3] USDA Forest Serv, Inst Pacific Isl Forestry, Hilo, HI USA
[4] Univ Calif Riverside, Dept Bot & Plant Sci, Riverside, CA USA
关键词
SURFACE-TEMPERATURE; GREEN SPACE; AIR; VEGETATION; CLIMATE; DEMAND; WATER;
D O I
10.1016/j.scs.2024.105677
中图分类号
TU [建筑科学];
学科分类号
0813 ;
摘要
Urban land cover types influence the urban microclimates. However, recent work indicates the magnitude of land cover's microclimate influence is affected by aridity. Moreover, this variation in cooling and warming potentials of urban land cover types can substantially alter the exposure of urban areas to extreme heat. Our goal is to understand both the relative influences of urban land cover on local air temperature, as well as how these influences vary during periods of extreme heat. To do so we apply predictive machine learning models to an extensive in-situ microclimate and 1 m land cover dataset across eight U.S. cities spanning a wide aridity gradient during typical and extreme heat conditions. We demonstrate how the cooling influence of tree canopy and the warming influence of buildings on microclimate linearly scales with regional aridity, while the influence of turf and impervious surfaces does not. These interactions lead tree canopy to consistently mitigate to air temperature increases during periods extreme heat in arid cities, while the influence of urban tree canopy on extreme heat in humid regions is varied, suggesting that mitigation is possible, but tree canopy can also aggravate extreme heat or have no significant effect.
引用
收藏
页数:13
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