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Article: Urbanization impact on meteorological condition and O3 concentration under past and future climates scenarios over the Greater Bay Area in Southern China

TitleUrbanization impact on meteorological condition and O3 concentration under past and future climates scenarios over the Greater Bay Area in Southern China
Authors
KeywordsClimate change
O3 concentration
Urban heat island
Urbanization
WRF-CAMx
Issue Date15-Aug-2024
PublisherElsevier
Citation
Atmospheric Environment, 2024, v. 331 How to Cite?
Abstract

Cities face twin challenges of changing climate and urban heat island (UHI) effect, with the environmental implications of urbanization still unclear. This study employs the Weather Research and Forecasting (WRF) model to examine the impacts of urbanization in the Greater Bay Area (GBA) during warm and cold seasons in past (2000) and near-future (2030) scenarios [i.e., under shared socioeconomic pathways (SSP): SSP1-26, SSP2-45, and SSP5-85]. Datasets from the World Urban Database and Access Portal Tools (WUDAPT) were incorporated into the WRF model to improve the representation of urbanization effects on weather patterns. Our findings indicate that urban expansion significantly increases urban temperatures and decreases wind speed across selected climate change scenarios. The spatially averaged urban temperatures in the fine resolution domain for 2030 could rise by 0.9 °C (warm season) and 2.4 °C (cold season), respectively, and urban wind speed decreases by ∼ 3 m/s under the SSP5-85 scenario. In cold season, the UHI effect could last over 20 h, while urban area may experience cooler nighttime temperatures than rural areas in warm season. Moreover, the future scenario predicts higher daytime O3 levels due to the warming effects of climate change and urbanization, but lower nighttime levels in warm season, attributed to intensified south-easterly sea breeze and background winds, when compared to the past scenario. This study highlights the importance of incorporating urbanization and climate change in future urban atmospheric environment studies, and underscores that urban climate change adaptation and mitigation should consider extra impacts on built-environment caused by urbanization.


Persistent Identifierhttp://hdl.handle.net/10722/347769
ISSN
2023 Impact Factor: 4.2
2023 SCImago Journal Rankings: 1.169

 

DC FieldValueLanguage
dc.contributor.authorWang, Qun-
dc.contributor.authorChen, Yiang-
dc.contributor.authorLu, Xingcheng-
dc.contributor.authorChen, Guangzhao-
dc.contributor.authorLi, Zhenning-
dc.contributor.authorCai, Meng-
dc.contributor.authorRen, Chao-
dc.contributor.authorFung, Jimmy CH-
dc.date.accessioned2024-09-28T00:30:27Z-
dc.date.available2024-09-28T00:30:27Z-
dc.date.issued2024-08-15-
dc.identifier.citationAtmospheric Environment, 2024, v. 331-
dc.identifier.issn1352-2310-
dc.identifier.urihttp://hdl.handle.net/10722/347769-
dc.description.abstract<p>Cities face twin challenges of changing climate and urban heat island (UHI) effect, with the environmental implications of urbanization still unclear. This study employs the Weather Research and Forecasting (WRF) model to examine the impacts of urbanization in the Greater Bay Area (GBA) during warm and cold seasons in past (2000) and near-future (2030) scenarios [i.e., under shared socioeconomic pathways (SSP): SSP1-26, SSP2-45, and SSP5-85]. Datasets from the World Urban Database and Access Portal Tools (WUDAPT) were incorporated into the WRF model to improve the representation of urbanization effects on weather patterns. Our findings indicate that urban expansion significantly increases urban temperatures and decreases wind speed across selected climate change scenarios. The spatially averaged urban temperatures in the fine resolution domain for 2030 could rise by 0.9 °C (warm season) and 2.4 °C (cold season), respectively, and urban wind speed decreases by ∼ 3 m/s under the SSP5-85 scenario. In cold season, the UHI effect could last over 20 h, while urban area may experience cooler nighttime temperatures than rural areas in warm season. Moreover, the future scenario predicts higher daytime O3 levels due to the warming effects of climate change and urbanization, but lower nighttime levels in warm season, attributed to intensified south-easterly sea breeze and background winds, when compared to the past scenario. This study highlights the importance of incorporating urbanization and climate change in future urban atmospheric environment studies, and underscores that urban climate change adaptation and mitigation should consider extra impacts on built-environment caused by urbanization.</p>-
dc.languageeng-
dc.publisherElsevier-
dc.relation.ispartofAtmospheric Environment-
dc.rightsThis work is licensed under a Creative Commons Attribution-NonCommercial-NoDerivatives 4.0 International License.-
dc.subjectClimate change-
dc.subjectO3 concentration-
dc.subjectUrban heat island-
dc.subjectUrbanization-
dc.subjectWRF-CAMx-
dc.titleUrbanization impact on meteorological condition and O3 concentration under past and future climates scenarios over the Greater Bay Area in Southern China-
dc.typeArticle-
dc.identifier.doi10.1016/j.atmosenv.2024.120585-
dc.identifier.scopuseid_2-s2.0-85193591335-
dc.identifier.volume331-
dc.identifier.eissn1878-2442-
dc.identifier.issnl1352-2310-

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