4.7 Article

Significant increase in extreme heat events along an urban-rural gradient

期刊

LANDSCAPE AND URBAN PLANNING
卷 215, 期 -, 页码 -

出版社

ELSEVIER
DOI: 10.1016/j.landurbplan.2021.104210

关键词

Urban climate; Heat wave; Within-city scale; Gradient analysis; Urban heat island; Urbanization

资金

  1. National Natural Science Foundation of China [41771203, SZCG2018261442]
  2. Shenzhen Municipal Ecology and Environment Bureau [SZCG2018161498, SZDL2020335165]
  3. Shenzhen Ecology and Environ-ment National Observation and Research Station

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Research has shown that extreme heat events (EHEs) exhibit significant spatial heterogeneity within cities, differing from the pattern of air temperature variations. The differences in EHEs between urban and non-urban areas are increasing significantly, with a faster growth rate in new urban areas compared to old urban areas. These findings can provide valuable insights for urban heat mitigation and adaptation strategies.
Cities worldwide are expecting more intense and frequent extreme heat events (EHEs) with climate change and urban growth. While previous studies have shown large intra-urban spatial variations in temperature, little is known regarding how EHEs were spatially distributed within a city. Here, taking Shenzhen, a rapidly urbanizing megacity in China as a case study, we examined the spatiotemporal pattern of EHEs, and further compared it with that of air temperature, using data collected from 85 weather stations from 2008 to 2017. We found: 1) Similar to air temperature, EHEs showed large spatial heterogeneity city-wide, which, however, was different from that of air temperature; 2) The differences in EHEs between urban and non-urban areas had significant increasing trends, with increasing rate of 0.50d/y (p < 0.01) of extreme heat day (EHD) and 1.23 h/y (p < 0.05) of extreme heat hour (EHH). In contrast, the increments of annual temperature differences between the two areas were negligible; 3) Increasing rates of EHEs in new urban areas (NUA) were more than twice those in old urban areas (OUA). Specifically, EHD, EHH, and heat wave increased at the rate of 0.79d/y, 3.20 h/y, and 0.22times/y in NUA, respectively, while the corresponding rates in OUA were 0.29d/y, 1.43 h/y, and 0.08times/y. These results can enhance our understanding of the within-city spatial heterogeneity of EHEs, and can therefore provide insights on urban heat mitigation and adaptation.

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