Satellite-Derived Subsurface Urban Heat Island
The subsurface urban heat island (SubUHI) is one part of the overall UHI specifying the relative warmth of urban ground temperatures against the rural background. To combat the challenge on measuring extensive underground temperatures with in situ instruments, we utilized satellite-based moderate-re...
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Published in | Environmental science & technology Vol. 48; no. 20; pp. 12134 - 12140 |
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Main Authors | , , , , , , , |
Format | Journal Article |
Language | English |
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Washington, DC
American Chemical Society
21.10.2014
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Abstract | The subsurface urban heat island (SubUHI) is one part of the overall UHI specifying the relative warmth of urban ground temperatures against the rural background. To combat the challenge on measuring extensive underground temperatures with in situ instruments, we utilized satellite-based moderate-resolution imaging spectroradiometer data to reconstruct the subsurface thermal field over the Beijing metropolis through a three-time-scale model. The results show the SubUHI’s high spatial heterogeneity. Within the depths shallower than 0.5 m, the SubUHI dominates along the depth profiles and analyses imply the moments for the SubUHI intensity reaching first and second extremes during a diurnal temperature cycle are delayed about 3.25 and 1.97 h per 0.1 m, respectively. At depths shallower than 0.05 m in particular, there is a subsurface urban cool island (UCI) in spring daytime, mainly owing to the surface UCI that occurs in this period. At depths between 0.5 and 10 m, the time for the SubUHI intensity getting to its extremes during an annual temperature cycle is lagged 26.2 days per meter. Within these depths, the SubUHI prevails without exception, with an average intensity of 4.3 K, varying from 3.2 to 5.3 K. |
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AbstractList | The subsurface urban heat island (SubUHI) is one part of the overall UHI specifying the relative warmth of urban ground temperatures against the rural background. To combat the challenge on measuring extensive underground temperatures with in situ instruments, we utilized satellite-based moderate-resolution imaging spectroradiometer data to reconstruct the subsurface thermal field over the Beijing metropolis through a three-time-scale model. The results show the SubUHI's high spatial heterogeneity. Within the depths shallower than 0.5 m, the SubUHI dominates along the depth profiles and analyses imply the moments for the SubUHI intensity reaching first and second extremes during a diurnal temperature cycle are delayed about 3.25 and 1.97 h per 0.1 m, respectively. At depths shallower than 0.05 m in particular, there is a subsurface urban cool island (UCI) in spring daytime, mainly owing to the surface UCI that occurs in this period. At depths between 0.5 and 10 m, the time for the SubUHI intensity getting to its extremes during an annual temperature cycle is lagged 26.2 days per meter. Within these depths, the SubUHI prevails without exception, with an average intensity of 4.3 K, varying from 3.2 to 5.3 K. |
Author | Hai, Shuoping Ju, Weimin Tang, Chaosheng Guo, Zhen Kong, Fanhua Zhan, Wenfeng Ferguson, Grant Quan, Jinling |
AuthorAffiliation | Beijing Normal University State Key Laboratory of Earth Surface Processes and Resource Ecology Service Center for China Meteorological Administration National Satellite Meteorological Center School of Earth Sciences and Engineering Jiangsu Provincial Key Laboratory of Geographic Information Science and Technology, International Institute of Earth System Science Department of Civil and Geological Engineering University of Saskatchewan Nanjing University |
AuthorAffiliation_xml | – name: School of Earth Sciences and Engineering – name: Service Center for China Meteorological Administration – name: – name: Nanjing University – name: Department of Civil and Geological Engineering – name: State Key Laboratory of Earth Surface Processes and Resource Ecology – name: National Satellite Meteorological Center – name: Beijing Normal University – name: University of Saskatchewan – name: Jiangsu Provincial Key Laboratory of Geographic Information Science and Technology, International Institute of Earth System Science |
Author_xml | – sequence: 1 givenname: Wenfeng surname: Zhan fullname: Zhan, Wenfeng email: zhanwenfeng@foxmail.com organization: Beijing Normal University – sequence: 2 givenname: Weimin surname: Ju fullname: Ju, Weimin – sequence: 3 givenname: Shuoping surname: Hai fullname: Hai, Shuoping organization: Service Center for China Meteorological Administration – sequence: 4 givenname: Grant surname: Ferguson fullname: Ferguson, Grant organization: University of Saskatchewan – sequence: 5 givenname: Jinling surname: Quan fullname: Quan, Jinling organization: Beijing Normal University – sequence: 6 givenname: Chaosheng surname: Tang fullname: Tang, Chaosheng – sequence: 7 givenname: Zhen surname: Guo fullname: Guo, Zhen organization: National Satellite Meteorological Center – sequence: 8 givenname: Fanhua surname: Kong fullname: Kong, Fanhua |
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Keywords | Spectroradiometry Moderate resolution imaging spectroradiometer Megacity Space remote sensing Satellite observation urban areas Microclimate Urban heat island Urban climate |
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SubjectTerms | Cities - statistics & numerical data Convection, turbulence, diffusion. Boundary layer structure and dynamics Earth, ocean, space Environmental Monitoring Exact sciences and technology External geophysics Heat Hot Temperature Meteorology Models, Theoretical Remote Sensing Technology Rural areas Seasons Temperature Urban heat islands |
Title | Satellite-Derived Subsurface Urban Heat Island |
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