Urban green space and albedo impacts on surface temperature across seven United States cities

被引:22
|
作者
Smith, Ian A. [1 ]
Fabian, M. Patricia [2 ]
Hutyra, Lucy R. [1 ]
机构
[1] Boston Univ, Dept Earth & Environm, 685 Commonwealth Ave, Boston, MA 02215 USA
[2] Boston Univ, Dept Environm Hlth, 715 Albany St, Boston, MA 02118 USA
基金
美国国家科学基金会;
关键词
Urban greening; White roofs; Albedo; Surface temperature; Urban heat island; Climate change; Climate adaptation; Heat exposure; HEAT; TREES; EVAPOTRANSPIRATION; GRADIENTS; SATELLITE; COMMUNITY; STRESS; METRO; WHITE; ROOFS;
D O I
10.1016/j.scitotenv.2022.159663
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
Extreme heat represents a growing threat to public health, especially across the densely populated, developed landscape of cities. Climate adaptation strategies that aim to manage urban microclimates through purposeful design can reduce the heat exposure of urban populations, however, it is unclear how the temperature impacts of urban green space and albedo vary across cities and background climate. This study quantifies the sensitivity of surface temperature to landcover characteristics tied to two widely used climate adaptation strategies, urban greening and albedo manipulation (e.g. white roofs), by combining long-term remote sensing observations of land surface temperature, albedo, and moisture with high-resolution landcover datasets in a spatial regression analysis at the census block scale across seven United States cities. We find tree cover to have an average cooling impact of -0.089 K per % cover, which is approximately four times stronger than the average grass cover cooling impact of -0.021 K per % cover. Variability in the magnitude of grass cover cooling impacts was primarily a function of vegetation moisture content, with the Land Surface Water Index (LSWI) explaining 89 % of the variability in grass cover cooling impacts across cities. Variability in tree cover cooling impacts was primarily a function of sunlight and vegetation moisture content, with solar irradiance and LSWI explaining 97 % of the cooling variability across cities. Albedo cooling impacts were consistent across cities with an average cooling impact of -0.187 K per increase of 0.01. While these interventions are broadly effective across cities, there are critical regional trade-offs between vegetation cooling efficiency, irrigation requirements, and the temporal duration and evolution of the cooling benefits. In warm, arid cities, high albedo surfaces offer multifaceted benefits such as cooling and water conservation, whereas temperate, mesic cities likely benefit from a combination of strategies, with greening efforts targeting highly paved neighborhoods.
引用
收藏
页数:12
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