| Literature DB >> 36011887 |
SangHyeok Lee1, Donghyun Kim2.
Abstract
With the global acceleration of urbanization, temperatures in cities are rising continuously with global climate change, creating an imminent risk of urban heat islands and urban heating. Although much research has attempted to analyze urban heating from various perspectives, a comprehensive approach to urban planning that addresses the problem is just beginning. This study suggests a conceptual framework for multidisciplinary understanding of urban heating by reviewing 147 selected articles from various fields, published between 2007 and 2021, that discuss urban heating mitigation. From these, we identified several outdoor and indoor temperature-reduction factors and proposed area-based, zoning-based, and point-based approaches to mitigate urban heating.Entities:
Keywords: heatwave; urban heat island; urban heating mitigation
Mesh:
Year: 2022 PMID: 36011887 PMCID: PMC9407880 DOI: 10.3390/ijerph191610249
Source DB: PubMed Journal: Int J Environ Res Public Health ISSN: 1660-4601 Impact factor: 4.614
Effects of vegetation, green spaces, and trees on mitigating urban heating.
| Research | Main Results | Area |
|---|---|---|
| Klok et al. [ | Green space accounts for 69% of temperature change. | Rotterdam |
| Guo et al. [ | Normalized Difference Vegetation Index (NDVI) and Land Surface Temperature (LST) show a strong negative correlation. | Guangzhou |
| Heusinkveld et al. [ | Green space reduces temperature by 4.0 K in urban areas. | Rotterdam |
| Wang et al. [ | A 10% increase in vegetation cover in urban areas lowers mean air temperature by 0.5–0.8 °C. | Toronto |
| Peron et al. [ | Replacing existing cover with cool materials and pervious green spaces lowers temperature by 4 °C. | Venice |
| Li et al. [ | A 10% increase in green space lowers LST by 0.86 °C. | Beijing |
| Sung [ | There is a strong negative correlation between the ratio of tree-covered area and mean surface temperature. | Woodland (Texas) |
| Chow et al. [ | Green space lowers temperature by 1–3 °C, and sometimes by up to 5 °C. | Phoenix |
| Klemm et al. [ | A 10% increase in tree planting lowers mean temperature in urban canyons by 1 K. | Utrecht |
| Armson et al. [ | Green space reduces surface temperature in urban areas by 20 °C maximum, and tree shade lowers overall temperature by 5–7 °C. | Manchester |
| Coutts and Harris [ | A 10% increase in vegetation cover lowers surface temperature by approximately 1 °C. | Melbourne |
| Qiu et al. [ | Green space in urban areas mitigates UHI intensity by 1.57 °C. | Shenzhen |
| Zölch et al. [ | Maximum saturation of tree planting can lower Physiological Equivalent Temperature (PET) by up to 10–13%. | Munich |
| Middel et al. [ | A 25% increase in urban tree canopy cover lowers air temperature by 2 °C. | Phoenix |
| Sun and Chen [ | The effect of green spaces on surface temperature is 1.64 °C for forests and 2.21 °C for lawns. | Beijing |
| Zhang, Murray et al. [ | Increasing green spaces lowers LST by approximately 1–2 °C locally, and by 0.5 °C regionally. | Phoenix |
| Park et al. [ | Polygonal and mixed type small green spaces lower temperature by 1 °C per 300 m2 area and 2300 m3 volume, and 2 °C per 650 m2 area and 5000 m3 volume. | Seoul |
| Ng et al. [ | Lowering the temperature of an urban area by 1 °C requires tree planting in 33% of that area. | Hong Kong |
| Tan et al. [ | In contrast to exposed surfaces, tree shade on the road lowers air temperature by 15.9–18.8 °C, and 1–1.5 °C at the pedestrian level. | Hong Kong |
| Hamada and Ohta [ | The maximum temperature difference between urban areas and green spaces is 1.9 °C. | Nagoya |
| Lee et al. [ | The mean temperature difference between urban areas and green spaces is 1.76 °C. | Seoul |
| Wang and Shu [ | A 10–20% increase in vegetation cover is anticipated to reduce UHI by 0.38–0.78 °C. | Shanghai |
| Dutta et al. [ | Green park has a cooling effect of 0.938 °C up to 50 m from the boundary, and 0.283 °C lower on average at 50–100 m. | India |
| Dialesandro et al. [ | Urban forest landscape cools daytime temperatures by 5.6 °C compared to the metropolitan average. | Dryland urban regions |
| Gao et al. [ | The maximum cooling effect of green roof is 1–1.2 K. | Xi’an and Wuhan |
| Žuvela-Aloise et al. [ | 0.5 °C can be reduced if all roofs in the entire area are changed to green roofs. | Vienna |
| Shah et al. [ | The average temperature difference between urban areas and green spaces is 2.23 °C. | Bengaluru |
| Bianchi et al. [ | The UHI effect in urban areas is due to hot exhaust gas from traffic, asphalt, and concentration of soot (no vegetation area). | Salt Lak Valley (Utah) |
| Zinzi and Carnielo [ | The UHI effect ranges between 0.7 and 1.8 °C and a maximum of 8.1 °C hourly. The large vegetation areas take advantage of evaporative cooling. | Rome |
| Street et al. [ | The energy use intensity of urban areas (little vegetation) is higher than that of rural areas (13% for a small office, 17% for a single family). | Boston |
Note: We added three articles (#77–#79) during the review process. Article #77 is not included in the index of Web of Science, and article #79 is a conference article.
Figure 1Comprehensive framework for understanding urban heating in urban planning.