4.7 Article

Temporal characteristics of urban heat island and its response to heat waves and energy consumption in the mountainous Chongqing, China

期刊

SUSTAINABLE CITIES AND SOCIETY
卷 75, 期 -, 页码 -

出版社

ELSEVIER
DOI: 10.1016/j.scs.2021.103260

关键词

Urban heat island; Temporal characteristics; Heat waves; Cooling degree days; Heating degree days; Mountainous city

资金

  1. National Natural Science Foundation of China [51708054, 52078075]
  2. Chengdu Science and Technology Project
  3. Fundamental Research Funds for the Central Universities [2018CDXYCH0015]

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The study conducted a statistical analysis of the temperature time series in Chongqing, China from 1979 to 2018, focusing on the urban heat island intensity (UHII) interdecadal and seasonal variation characteristics. Results indicated a significant rise in temperature in Chongqing over the past 40 years, with the urban area experiencing a temperature approximately 1.6 times higher than the global warming trend. The study also found a significant increase in annual average UHII at urban and rural stations, with higher seasonal variation in nighttime UHII during summer and daytime UHII during winter. Furthermore, the annual average UHII was related to heat wave days, cooling degree days, and heating degree days, with each 1 degree C increase in UHII leading to specific changes in these parameters.
In this study, the time series of temperature in Chongqing, China, from 1979 to 2018 was statistically analyzed, and both the interdecadal and seasonal variation characteristics of urban heat island intensity (UHII) were studied. The results show that the temperature in Chongqing has risen significantly in the past 40 years and that the temperature of the Chongqing urban area is approximately 1.6 times higher than the global warming trend. During the study period, the annual average UHII at urban and rural stations increased significantly at a rate of +1.3 degrees C/century. The seasonal variation in the nighttime UHII was higher in summer, while the seasonal variation in the daytime UHII was higher in winter. In addition, the annual average UHII was found to be related to the heat wave (HW) days, cooling degree days (CDD), and heating degree days (HDD). With an increase of 1 degrees C in the UHII, the HW days in urban area increased by approximately 10 d, the average difference of the CDD increased by approximately 72 degrees C center dot d, and the average difference of the HDD decreased by approximately 86 degrees C center dot d.

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