Vol.34,  No.1, 
December  2022
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Zhang Dejun, Yang Shiqi, Zhu Hao, et al. Quantitative evaluation of heat island effect in Chongqing metropolitan circle. J Appl Meteor Sci, 2023, 34(1): 91-103. DOI: 10.11898/1001-7313.20230108.
Citation: Zhang Dejun, Yang Shiqi, Zhu Hao, et al. Quantitative evaluation of heat island effect in Chongqing metropolitan circle. J Appl Meteor Sci, 2023, 34(1): 91-103. DOI: 10.11898/1001-7313.20230108.
shu

Quantitative Evaluation of Heat Island Effect in Chongqing Metropolitan Circle

  • 1.

    Chongqing Institute of Meteorological Sciences, Chongqing 401147

  • 2.

    Chongqing Engineering Research Center of Agrometeorology and Satellite Remote Sensing, Chongqing 401147

  • 3.

    Yilong Meteorological Bureau of Nanchong City, Sichuan Province, Nanchong 637000

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    Abstract
  • With global warming and rapid urbanization, urban climate is considered to be one important factor impacting urban ecological environment, and the most obvious feature of urban climate is the surface urban heat island(SUHI). The accurate division of rural reference area is critical in evaluating the intensity of SUHI in mountainous cities by urban-rural dichotomy. Therefore, a comprehensive method is proposed based on multi-source satellite remote sensing data to solve this problem, and the spatiotemporal variation of the SUHI in Chongqing metropolitan circle from 2001 to 2020 are analyzed. The results show that the spatial distribution of rural reference area obtained by the comprehensive buffer method is obviously different from that by the traditional buffer method, and the main cause is the limitation of the elevation difference between urban and rural reference area. There are a large number of "false SUHI" pixels in the SUHI product estimated by the traditional buffer method, which makes the surface urban heat island regions obtained by the traditional buffer method significantly larger than that by the comprehensive buffer method. The spatiotemporal distribution results show that the regions affected by the SUHI are concentrated in the core area of Chongqing, Changshou, Fuling and nearby regions, and the cold island are concentrated in the high-altitude areas in the southeast of Chongqing and some mountains in the core of Chongqing. The interannual variation of the SUHI shows that the proportion of areas above strong SUHI level increases with time from 2001 to 2020, and the SUHI is strong in summer and weak in winter. The proportion of strong SUHI area increased from 0.5% in 2001 to 2.95% in 2020, with an average annual growth rate of 0.12%. The proportion of intense heat island area increased from 0.21% in 2001 to 0.78% in 2019, with an average annual growth rate of 0.03%. The change of SUHI is closely related to urban development, and has a significant positive correlation with the economic driving factors such as the total population of the main city and metropolitan area, urban population, GDP, total energy consumption, urban built-up area and civil vehicle ownership. The correlation coefficients are 0.91, 0.94, 0.95, 0.94, 0.90 and 0.96, respectively, indicating that the driving factors of urban economy play an obvious role in promoting the change of SUHI intensity in the main metropolitan area.
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  • Fig  1.   Digital elevation and land-cover of the metropolitan circle of Chongqing

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    Fig  2.   Rural reference map of the metropolitan circle of Chongqing extracted at the scale from 5 km to 25 km based on traditional buffer algorithm and comprehensive buffer algorithm

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    Fig  3.   Rural reference areas of the metropolitan circle of Chongqing extracted at 25 km scale by traditional buffer algorithm and comprehensive buffer algorithm, city area and area of nighttime light great than 15 from 2001 to 2020

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    Fig  4.   Spatial distribution of the surface urban heat island in the metropolitan circle of Chongqing estimated by traditional buffer algorithm and comprehensive buffer algorithm

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    Fig  5.   Areas variation of the surface urban heat island in the metropolitan circle of Chongqing with buffer zone scale increasing from 5 km to 25 km in summer of 2020

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    Fig  6.   Areas of different surface urban heat island level in the metropolitan circle of Chongqing at different buffer zone scales in summer of 2020

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    Fig  7.   Annual spatial distribution of surface urban heat island in the metropolitan areas of Chongqing

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    Fig  8.   Area changes of surface urban heat island in the metropolitan areas of Chongqing from 2001 to 2020

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    Fig  9.   Seasonal spatial distribution of surface urban heat island in metropolitan circle of Chongqing in 2020

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    Fig  10.   Scatter plots of the economic factors and the areas of surface urban heat island in the metropolitan circle of Chongqing from 2001 to 2020

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    • Received : 2022-07-05
    • Accepted : 2022-10-08
    • Published : 2023-01-30
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