A global urban heat island intensity dataset: Generation, comparison, and analysis

被引:8
作者
Yang, Qiquan [1 ,2 ,3 ]
Xu, Yi [1 ]
Chakraborty, T. C. [4 ]
Du, Meng [5 ]
Hu, Ting [5 ]
Zhang, Ling [6 ]
Liu, Yue [7 ]
Yao, Rui [8 ]
Yang, Jie [8 ]
Chen, Shurui [2 ]
Xiao, Changjiang [2 ,3 ]
Liu, Renrui [1 ]
Zhang, Mingjie [1 ]
Chen, Rui [1 ]
机构
[1] Macau Univ Sci & Technol, State Key Lab Lunar & Planetary Sci, Macau, Peoples R China
[2] Tongji Univ, Coll Surveying & Geoinformat, Shanghai 200092, Peoples R China
[3] Tongji Univ, Shanghai Key Lab Space Mapping & Remote Sensing Pl, Shanghai 200092, Peoples R China
[4] Pacific Northwest Natl Lab, Atmospher Climate & Earth Sci Div, Richland, WA USA
[5] Nanjing Univ Informat Sci & Technol, Sch Remote Sensing & Geomat Engn, Nanjing 210044, Peoples R China
[6] Sun Yat Sen Univ, Sch Earth Sci & Engn, Guangzhou 510275, Peoples R China
[7] Guangdong Acad Sci, Guangzhou Inst Geog, Guangzhou 510070, Peoples R China
[8] Wuhan Univ, Sch Remote Sensing & Informat Engn, Wuhan 430079, Peoples R China
基金
中国国家自然科学基金;
关键词
Urban thermal environment; Urban warming trend; Rural definition; Estimation method; Spatiotemporal variation; LAND-SURFACE TEMPERATURE; 1 KM RESOLUTION; TEMPORAL TRENDS; CLIMATE; PATTERNS; CHINA; MODEL;
D O I
10.1016/j.rse.2024.114343
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
The urban heat island (UHI) effect, a phenomenon of local warming over urban areas, is the most well-known impact of urbanization on climate. Globally consistent estimates of the UHI intensity (UHII) are crucial for examining this phenomenon across time and space. However, publicly available UHII datasets are limited and have several constraints: (1) they are for clear-sky surface UHII, not all-sky surface UHII and canopy (air temperature) UHII; (2) the estimation methods often neglect anthropogenic disturbance, introducing uncertainties in the estimated UHII. To address these issues, this study proposes a new dynamic equal-area (DEA) method that can minimize the influence of various confounding factors on UHII estimates through a dynamic cyclic process. Utilizing the DEA method and leveraging various gridded temperature data, we develop a global-scale (>10,000 cities), long-term (over 20 years by month), and multi-faceted (clear-sky surface, all-sky surface, and canopy) UHII dataset. Based on these estimates, we provide a comprehensive analysis of the UHII and its trends in global cities. The UHII is found to be greater than zero in >80% of cities, with global annual average magnitudes around 1.0 degrees C (day) and 0.8 degrees C (night) for surface UHII, and close to 0.5 degrees C for canopy UHII. Furthermore, an interannual upward trend in UHII is observed in >60% of cities, with global annual average trends exceeding 0.1 degrees C/decade (day) and over 0.06 degrees C/decade (night) for surface UHII, and slightly surpassing 0.03 degrees C/decade for canopy UHII. Notably, there exists a positive correlation between the magnitude and trend of UHII, suggesting that cities with stronger UHII tend to experience faster growth in UHII. Additionally, discrepancies in UHII are found between different temperature data, stemming not only from distinctions in data types (surface or air temperature) but also from differences in data acquisition times (Terra or Aqua), weather conditions (clear-sky or all-sky), and processing methodologies (with or without gap filling). Overall, our proposed method, dataset, and analysis results have the potential to provide valuable insights for future urban climate studies. The UHII dataset is publicly available at https://doi.org/10.6084/m9.figshare.24821538.
引用
收藏
页数:23
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