Citation

Middel A, Krayenhoff ES. Sci. Total Environ. 2019; 687: 137-151.

Affiliation

Urban Climate Research Center, Arizona State University, 975 S Myrtle Ave, Tempe, AZ 85281, USA; School of Environmental Sciences, University of Guelph, 50 Stone Road East, Guelph, ON N1G 2W1, Canada. Electronic address: skrayenh@uoguelph.ca.

Copyright

(Copyright © 2019, Elsevier Publishing)

DOI

10.1016/j.scitotenv.2019.06.085

PMID

31207504

Abstract

We report the first set of urban micrometeorological measurements for assessment of pedestrian thermal exposure during extreme heat in a dry climate. Hourly measurements of air temperature, humidity, wind speed and six-directional shortwave and longwave radiation were recorded with a mobile human-biometeorological station (MaRTy) from 10:00 to 21:00 local time, June 19, 2016, at 22 sites that include diverse microscale urban land cover. Sky view factor (SVF) and 360° pervious and impervious view factors for each location were calculated from six-directional fisheye photographs. Mean radiant temperature (T_MRT) was determined using the six-directional method. Three-dimensional radiation budgets were decomposed into directional weighted shortwave and longwave radiation components to create a distinct T_MRT profile for each site and determine the main drivers of T_MRT and thermal exposure. Air temperature peaked locally at 48.5 °C, with a maximum T_MRT of 76.4 °C at 15:00 MST in an east-west building canyon. Longwave radiation measured by laterally-oriented sensors dominated the T_MRT budget, suggesting the importance of cooling vertical surfaces adjacent to pedestrians. Lateral shortwave radiation contributions were most spatially and temporally variable across T_MRT profiles, reflecting the diverse shade conditions. The largest radiation fluxes contributing to T_MRT were particularly sensitive to shade and secondarily to ground cover. Trees reduced afternoon T_MRT up to 33.4 °C but exhibited a clear T_MRT increase of up to 5 °C after sunset; during daytime, trees generated ground cover-dependent longwave radiant cooling or warming. Replacement of impervious with pervious ground cover cooled T_MRT at all measurement times, even under dense tree shade. While recent work has found that adaptation cannot offset projected urban air temperature increases, outdoor thermal exposure depends on additional micrometeorological variables, including shortwave and longwave radiation, indicating the need and the opportunity to create pedestrian spaces that are radiantly cool within the context of future urban heat.

Copyright © 2019 The Authors. Published by Elsevier B.V. All rights reserved.

Language: en

Keywords

Extreme heat; MaRTy; Mean radiant temperature; Microscale Urban Design; Radiation budget decomposition; Thermal comfort