Accessibility navigation


How do green roofs mitigate urban thermal stress under heat waves?

Downloads

Downloads per month over past year

Sun, T., Grimmond, C. S. E. and Ni, G.-H. (2016) How do green roofs mitigate urban thermal stress under heat waves? Journal of Geophysical Research: Atmospheres, 121 (10). pp. 5320-5335. ISSN 2169-8996

[img]
Preview
Text - Published Version
· Please see our End User Agreement before downloading.

6MB
[img] Text (Permanent Publisher Embargo) - Accepted Version
· Restricted to Repository staff only

2MB

To link to this item DOI: 10.1002/2016JD024873

Abstract/Summary

As the climate warms, heat waves (HW) are projected to be more intense and to last longer, with serious implications for public health. Urban residents face higher health risks because urban heat islands (UHIs) exacerbate HW conditions. One strategy to mitigate negative impacts of urban thermal stress is the installation of green roofs (GRs) given their evaporative cooling effect. However, the effectiveness of GRs and the mechanisms by which they have an effect at the scale of entire cities are still largely unknown. The Greater Beijing Region (GBR) is modeled for a HW scenario with the Weather Research and Forecasting (WRF) model coupled with a state-of-the-art urban canopy model (PUCM) to examine the effectiveness of GRs. The results suggest GR would decrease near-surface air temperature (ΔT2max = 2.5 K) and wind speed (ΔUV10max = 1.0 m s-1) but increase atmospheric humidity (ΔQ2max = 1.3 g kg-1). GRs are simulated to lessen the overall thermal stress as indicated by apparent temperature (ΔAT2max = 1.7 °C). The modifications by GRs scale almost linearly with the fraction of the surface they cover. Investigation of the surface-atmosphere interactions indicate that GRs with plentiful soil moisture dissipate more of the surface energy as latent heat flux and subsequently inhibit the development of the daytime planetary boundary layer (PBL). This causes the atmospheric heating through entrainment at the PBL top to be decreased. Additionally, urban GRs modify regional circulation regimes leading to decreased advective heating under HW.

Item Type:Article
Refereed:Yes
Divisions:Faculty of Science > School of Mathematical, Physical and Computational Sciences > Department of Meteorology
ID Code:65530
Publisher:American Geophysical Union

University Staff: Request a correction | Centaur Editors: Update this record

Page navigation