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Summer Cooling Effect of Rivers in the Yangtze Basin, China: Magnitude, Threshold and Mechanisms

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  • Pan Xiong

    (School of Smart City, Chongqing Jiaotong University, No. 66 Xuefu Rd., Nan’an Dist., Chongqing 400074, China
    These authors contributed equally to this work.)

  • Dongjie Guan

    (School of Smart City, Chongqing Jiaotong University, No. 66 Xuefu Rd., Nan’an Dist., Chongqing 400074, China)

  • Yanli Su

    (School of Smart City, Chongqing Jiaotong University, No. 66 Xuefu Rd., Nan’an Dist., Chongqing 400074, China
    These authors contributed equally to this work.)

  • Shuying Zeng

    (School of Smart City, Chongqing Jiaotong University, No. 66 Xuefu Rd., Nan’an Dist., Chongqing 400074, China
    These authors contributed equally to this work.)

Abstract

Under the dual pressures of global climate warming and rapid urbanization, the Yangtze River Basin, as the world’s largest urban agglomeration, is facing intensifying thermal environmental stress. Although river ecosystems demonstrate significant thermal regulation functions, their spatial thresholds of cooling effects and multiscale driving mechanisms have remained to be systematically elucidated. This study retrieved land surface temperature (LST) using the split window algorithm and quantitatively analyzed the changes in the river cold island effect and its driving mechanisms in the Yangtze River Basin by combining multi-ring buffer analysis and the optimal parameter-based geographical detector model. The results showed that (1) forest land is the main land use type in the Yangtze River Basin, with built-up land having the largest area increase. Affected by natural, socioeconomic, and meteorological factors, the summer temperatures displayed a spatial pattern of “higher in the east than the west, warmer in the south than the north”. (2) There are significant differences in the cooling magnitude among different land types. Forest land has the maximum daytime cooling distance (589 m), while construction land has the strongest cooling magnitude (1.72 °C). The cooling effect magnitude is most pronounced in upstream areas of the basin, reaching 0.96 °C. At the urban agglomeration scale, the Chengdu–Chongqing urban agglomeration shows the greatest temperature reduction of 0.90 °C. (3) Elevation consistently demonstrates the highest explanatory power for LST spatial variability. Interaction analysis shows that the interaction between socioeconomic factors and elevation is generally the strongest. This study provides important spatial decision support for formulating basin-scale ecological thermal regulation strategies based on refined spatial layout optimization, hierarchical management and control, and a “natural–societal” dual-dimensional synergistic regulation system.

Suggested Citation

  • Pan Xiong & Dongjie Guan & Yanli Su & Shuying Zeng, 2025. "Summer Cooling Effect of Rivers in the Yangtze Basin, China: Magnitude, Threshold and Mechanisms," Land, MDPI, vol. 14(8), pages 1-27, July.
  • Handle: RePEc:gam:jlands:v:14:y:2025:i:8:p:1511-:d:1707524
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    References listed on IDEAS

    as
    1. Huawei Li & Sandor Jombach & Guohang Tian & Yuanzheng Li & Handong Meng, 2022. "Characterizing Temporal Dynamics of Urban Heat Island in a Rapidly Expanding City: A 39 Years Study in Zhengzhou, China," Land, MDPI, vol. 11(10), pages 1-18, October.
    2. Jiqing Lin & Wufa Yang & Kunyong Yu & Jianwei Geng & Jian Liu, 2023. "Construction of Water Corridors for Mitigation of Urban Heat Island Effect," Land, MDPI, vol. 12(2), pages 1-18, January.
    3. Jiaxing Xin & Jun Yang & Dongqi Sun & Tianyu Han & Chunrui Song & Zhipeng Shi, 2022. "Seasonal Differences in Land Surface Temperature under Different Land Use/Land Cover Types from the Perspective of Different Climate Zones," Land, MDPI, vol. 11(8), pages 1-17, July.
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