Variation the in relationship between urban tree canopy and air temperature reduction under a range of daily weather conditions

被引:4
作者
Locke, Dexter Henry [1 ]
Baker, Matthew [2 ]
Alonzo, Michael [3 ]
Yang, Yichen [4 ]
Ziter, Carly D. [5 ]
Murphy-Dunning, Colleen [6 ]
O'Neil-Dunne, Jarlath P. M. [7 ]
机构
[1] USDA Forest Serv, Northern Res Stn, Baltimore Field Stn, Suite 350,5523 Res Pk Dr, Baltimore, MD 21228 USA
[2] Univ Maryland Baltimore Cty, Dept Geog & Environm Syst, 1000 Hilltop Circle, Baltimore, MD 21250 USA
[3] Amer Univ, Dept Environm Sci, Hall Sci 328 4400 Massachusetts Ave, Washington, DC 20016 USA
[4] Environm Sci Ctr, Yale Sch Environm, Room 300, 21 Sachem St, New Haven, CT 06511 USA
[5] Concordia Univ, Dept Biol, 7141 Sherbrooke West, Montreal, PQ H4B 1R6, Canada
[6] Yale Sch Environm, Hixon Ctr Urban Sustainabilitiy, Urban Resources Initiat, 301 Prospect St 1, New Haven, CT 06511 USA
[7] Univ Vermont, Rubenstein Sch Environm & Nat Resources, Spatial Anal Lab, 81 Carrigan Dr, Burlington, VT 05405 USA
关键词
Urban heat island; Mobile sampling; Distributed network; Air temperature; Bicycles; Tree canopy; HEAT-ISLAND; LAND; CITY; VARIABILITY; SIZE;
D O I
10.1016/j.heliyon.2024.e25041
中图分类号
O [数理科学和化学]; P [天文学、地球科学]; Q [生物科学]; N [自然科学总论];
学科分类号
07 ; 0710 ; 09 ;
摘要
Mitigating heat is a vital ecosystem service of trees, particularly with climate change. Land surface temperature measures captured at a single time of day (in the morning) dominate the urban heat island literature. Less is known about how local tree canopy and impervious surface regulate air temperature throughout the day, and/or across many days with varied weather conditions, including cloud cover. We use bike-mounted air temperature sensors throughout the day in New Haven, Connecticut, USA, from 2019 to 2021 and generalized additive mixed models across 156 rides to estimate the daily variation in cooling benefits associated with tree canopy cover, and warming from impervious surface cover in 90 m buffers surrounding bike observations. Cooling is inferred by subtracting the bicycle-observed temperature from a reference station. The cooling benefits from tree canopy cover were strongest in the midday (11:00-14:00, -1.62 degrees C), afternoon (14:00-17:00, -1.19 degrees C), and morning (8:00-11:00, -1.15 degrees C) on clear days. The cooling effect was comparatively smaller on cloudy mornings -0.92 degrees C and afternoons -0.51 degrees C. Warming from impervious surfaces was most pronounced in the evening (17:00-20:00, 1.11 degrees C) irrespective of clouds, and during cloudy nights (20:00-23:00) and cloudy mornings 1.03 degrees C 95 % CI [1.03, 1.04]. Among the hottest observed days (top 25th percentile of reference station daily maxima), tree canopy was associated with lower temperatures on clear afternoons -1.78 degrees C [-1.78, -1.78], cloudy midday -1.17 degrees C [-1.19, -1.15], clear midday -1.12 degrees C [-1.12, -1.11]. We add a broader spectrum of weather conditions by explicitly including clouds, and greater temporal resolution by measuring throughout the day to bike-based urban heat research. Future mobile sampling campaigns may broaden the spatial extent with more environmental variation, representing an opportunity for public science and engagement.
引用
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页数:12
相关论文
共 54 条
[1]   Spatial configuration and time of day impact the magnitude of urban tree canopy cooling [J].
Alonzo, Michael ;
Baker, Matthew E. ;
Gao, Yuemeng ;
Shandas, Vivek .
ENVIRONMENTAL RESEARCH LETTERS, 2021, 16 (08)
[2]   Measurement and Statistical Modeling of the Urban Heat Island of the City of Utrecht (the Netherlands) [J].
Brandsma, Theo ;
Wolters, Dirk .
JOURNAL OF APPLIED METEOROLOGY AND CLIMATOLOGY, 2012, 51 (06) :1046-1060
[3]   Performance Evaluation of a Smart Mobile Air Temperature and Humidity Sensor for Characterizing Intracity Thermal Environment [J].
Cao, Chang ;
Yang, Yichen ;
Lu, Yang ;
Schultze, Natalie ;
Gu, Pingyue ;
Zhou, Qi ;
Xu, Jiaping ;
Lee, Xuhui .
JOURNAL OF ATMOSPHERIC AND OCEANIC TECHNOLOGY, 2020, 37 (10) :1891-1905
[4]   Urban expansion weakens the contribution of local land cover to urban warming [J].
Cao, Jie ;
Zhou, Weiqi ;
Yu, Wenjuan ;
Hu, Xiaofang ;
Yu, Miao ;
Wang, Jing ;
Wang, Jia .
URBAN CLIMATE, 2022, 45
[5]   Mobile measurements of microclimatic variables through the central area of Singapore: An analysis from the pedestrian perspective [J].
Chafer, Marta ;
Tan, Chun Liang ;
Cureau, Roberta Jacoby ;
Hien, Wong Nyuk ;
Pisello, Anna Laura ;
Cabeza, Luisa F. .
SUSTAINABLE CITIES AND SOCIETY, 2022, 83
[6]   Residential segregation and outdoor urban moist heat stress disparities in the United States [J].
Chakraborty, T. C. ;
Newman, Andrew J. ;
Qian, Yun ;
Hsu, Angel ;
Sheriff, Glenn .
ONE EARTH, 2023, 6 (06) :738-750
[7]   NEW METHOD OF AIR-TEMPERATURE MEASUREMENT IN URBAN CLIMATOLOGICAL STUDIES [J].
CONRADS, LA ;
VANDERHA.JC .
ATMOSPHERIC ENVIRONMENT, 1971, 5 (08) :629-&
[8]   Effects of urban tree canopy loss on land surface temperature magnitude and timing [J].
Elmes, Arthur ;
Rogan, John ;
Williams, Christopher ;
Ratick, Samuel ;
Nowak, David ;
Martin, Deborah .
ISPRS JOURNAL OF PHOTOGRAMMETRY AND REMOTE SENSING, 2017, 128 :338-353
[9]   Contributions of roads to surface temperature: evidence from Southern California [J].
Engel, Ruth A. ;
Millard-Ball, Adam ;
Turner, V. Kelly .
ENVIRONMENTAL RESEARCH COMMUNICATIONS, 2023, 5 (01)
[10]  
Epstien P.R., 2005, Climate Change Futures: Health, Ecological and Economic Dimensions