Effects of heat storage on urban thermal environment and surface energy balance by scaled outdoor experiments

• The impact of heat storage on urban thermal environment and energy balance is studied. • Increasing heat storage ( Δ Q S ) reduces the daily temperature range ( DTR ). • As the cloud cover increases, the effect of Δ Q S on DTR weakens. • The impact of sky conditions on Δ Q S / Q * (heat storage/net radiation) is minimal. • Δ Q S / Q * shows a clear negative correlation with friction velocity ( u * ). Heat storage ( Δ Q S ) is a crucial component of the urban surface energy balance (USEB) and urban thermal environment. However, the estimation of Δ Q S in real urban environments is associated with significant uncertainty. As a novelty, we conducted a scaled outdoor experiment to investigate the impact of Δ Q S on the urban thermal environment and USEB under different sky conditions. The experiment performed a comparative analysis using Case Water (water models with high thermal mass) and Case Hollow (hollow models with low thermal mass). Compared with Case Hollow, the daily heat storage in Case Water increases by 0.26 MJm −2 day −1 , resulting in a lower daily temperature range ( DTR ). The difference in DTR between Case Water and Case Hollow is 3.6 °C (clear sky), 2.8 °C (partially cloudy sky), and 1.4 °C (cloudy sky). As the cloud cover increases, the effect of increased Δ Q S in reducing DTR becomes less significant. The impact of sky conditions on Δ Q S / Q * (heat storage/net radiation) is minimal (37.5 %, 37.8 %, 35.6 % for clear sky, partially cloudy sky and cloudy sky, respectively). Furthermore, Δ Q S / Q * shows a clear negative correlation with friction velocity ( u * ), with the influence of u * becoming more pronounced as the cloud cover increases. u * explains approximately 30 % of the variation in Δ Q S / Q * . This study enhances our understanding of how Δ Q S influences the urban thermal environment, while also providing high-quality data to support numerical simulations and theoretical models.

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Publication Details

Journal
Building and Environment
Published
2025-04-02
DOI
https://doi.org/10.1016/j.buildenv.2025.112952
Citations
3
Primary Topic
Urban Heat Island Mitigation
Type
article
Field-Weighted Citation Impact
2.40
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article

Effects of heat storage on urban thermal environment and surface energy balance by scaled outdoor experiments

Jian Hang, Guanwen Chen, Longhao Ren, Liyue Zeng et al.
3 citations
Building and Environment
Urban Heat Island Mitigation
2.40
article

Effects of heat storage on urban thermal environment and surface energy balance by scaled outdoor experiments

Jian Hang, Guanwen Chen, Longhao Ren, Liyue Zeng, Hua Dong, Yuguang Zhao, Shaojia Fan, Na Zhao, Hua Yuan
article en
3 citations

Abstract

• The impact of heat storage on urban thermal environment and energy balance is studied. • Increasing heat storage ( Δ Q S ) reduces the daily temperature range ( DTR ). • As the cloud cover increases, the effect of Δ Q S on DTR weakens. • The impact of sky conditions on Δ Q S / Q * (heat storage/net radiation) is minimal. • Δ Q S / Q * shows a clear negative correlation with friction velocity ( u * ). Heat storage ( Δ Q S ) is a crucial component of the urban surface energy balance (USEB) and urban thermal environment. However, the estimation of Δ Q S in real urban environments is associated with significant uncertainty. As a novelty, we conducted a scaled outdoor experiment to investigate the impact of Δ Q S on the urban thermal environment and USEB under different sky conditions. The experiment performed a comparative analysis using Case Water (water models with high thermal mass) and Case Hollow (hollow models with low thermal mass). Compared with Case Hollow, the daily heat storage in Case Water increases by 0.26 MJm −2 day −1 , resulting in a lower daily temperature range ( DTR ). The difference in DTR between Case Water and Case Hollow is 3.6 °C (clear sky), 2.8 °C (partially cloudy sky), and 1.4 °C (cloudy sky). As the cloud cover increases, the effect of increased Δ Q S in reducing DTR becomes less significant. The impact of sky conditions on Δ Q S / Q * (heat storage/net radiation) is minimal (37.5 %, 37.8 %, 35.6 % for clear sky, partially cloudy sky and cloudy sky, respectively). Furthermore, Δ Q S / Q * shows a clear negative correlation with friction velocity ( u * ), with the influence of u * becoming more pronounced as the cloud cover increases. u * explains approximately 30 % of the variation in Δ Q S / Q * . This study enhances our understanding of how Δ Q S influences the urban thermal environment, while also providing high-quality data to support numerical simulations and theoretical models.

Building and EnvironmentVol. 277
Sun Yat-sen University (CN), Southern Marine Science and Engineering Guangdong Laboratory (Guangzhou) (CN), Hebei Meteorological Bureau (CN), Southern Marine Science and Engineering Guangdong Laboratory (Zhuhai) (CN), Xingtai University (CN)
Sustainable cities and communities
Openalex Percentile: Top 13%
Urban Heat Island Mitigation
2.40
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