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城市热浪与冠层热岛协同作用研究进展与展望

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城市化的加速和人口聚集不仅加剧了城市冠层热岛效应,还影响高温热浪事件,二者的叠加效应将严重影响城市发展和居民健康.目前部分研究认为热浪与热岛之间存在协同加强的变化特征,但是热浪与城市热岛的叠加效应仍存在较大差异性.通过全面回顾和总结国内外关于热浪与热岛协同作用差异性方面的研究,并从气候背景、局地环流以及城市形态等方面探讨了城市高温的形成机制.在不同气候背景和局地环流条件下,热浪与热岛协同作用呈现出显著的时空差异性,尤其是局地环流的调节作用不可忽视.近10年提出的局地气候区分类在热浪与热岛协同作用方面的研究已经取得了一些成果,但是有必要从城市三维形态方面入手进一步探索其响应特征.目前,未统一标准的热浪定义对深入理解热浪—城市热岛相互作用带来了不确定性.当下需要更全面地了解热浪和热岛带来的城市过度变暖的时空差异性及其形成机制和调节因素,为高温监测和城市居住环境改善提供更详细的指导和理论支撑.
Research Progress and Perspective on Synergy Between Urban Heat Waves and Canopy Urban Heat Island
The acceleration of urbanization and population agglomeration intensifies the Urban Heat Island(UHI)effect and causes Heat Waves(HWs).The superimposed effects of the two seriously affect urban development and resident health.A few studies believe that HWs and UHI intensity have the characteristics of synergistic enhancement,but there are still large differences in the superimposed effects of HW-UHI.This article comprehensively reviews and summarizes domestic and foreign research on the differences in the synergy between HWs and UHI and explores the formation mechanism of urban high temperatures from the aspects of climate background,local circulation,and urban morphology.Under different climatic backgrounds and local circulation conditions,the synergistic effects of the HW-UHI show significant spatiotemporal differences,particularly the regulatory role of local circulation,which cannot be ignored.The Local Climate Zone(LCZs)classification proposed in the past decade has achieved some results in research on the synergy between HWs and UHI;however,it is necessary to further explore their response characteristics from the three-dimensional morphology of the city.Currently,there is no unified standard definition for HWs,which brings uncertainty to an in-depth understanding of HW-UHI interactions.There is a need to comprehensively understand the spatiotemporal differences in excessive urban warming caused by HW and UHI and their formation mechanisms and regulating factors to provide more detailed guidance and theoretical support for high-temperature monitoring and improvement of the urban living environment.

Urban heat islandHeat waveSynergyDifferenceDriving factorsUrban microclimate

杨元建、罗芙、薛捷升、宗莲、田伟守、石涛

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南京信息工程大学大气物理学院,江苏 南京 210044

芜湖市气象局,安徽 芜湖 241000

城市热岛 高温热浪 协同作用 差异性 驱动因子 城市微气候

国家自然科学基金项目国家自然科学基金项目中国气象局气象能力提升联合研究专项中国气象局气象能力提升联合研究专项

42222503421051474222250342105147

2024

地球科学进展
中国科学院资源环境科学信息中心 国家自然科学基金委员会地球科学部 中国科学院资源环境科学与技术局

地球科学进展

CSTPCD北大核心
影响因子:2.045
ISSN:1001-8166
年,卷(期):2024.39(4)
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