Warming and cooling effects of local climate zones on urban thermal environment
Understanding the thermal characteristics and contribution ranking of local climate zones (LCZs) is essential since they can help in maintaining environmental harmony. However, previous studies only considered independent effects and could not analyze the combined effects of LCZ on land surface temp...
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Frontiers Media S.A.
2022-11-01
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Series: | Frontiers in Public Health |
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Online Access: | https://www.frontiersin.org/articles/10.3389/fpubh.2022.1072174/full |
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author | Rui Zhang Jun Yang Jun Yang Jun Yang Dongqi Sun Xinyue Ma Wenbo Yu Xiangming Xiao Jianhong (Cecilia) Xia |
author_facet | Rui Zhang Jun Yang Jun Yang Jun Yang Dongqi Sun Xinyue Ma Wenbo Yu Xiangming Xiao Jianhong (Cecilia) Xia |
author_sort | Rui Zhang |
collection | DOAJ |
description | Understanding the thermal characteristics and contribution ranking of local climate zones (LCZs) is essential since they can help in maintaining environmental harmony. However, previous studies only considered independent effects and could not analyze the combined effects of LCZ on land surface temperature (LST). In this study, we propose a new method to establish an interaction model between LCZs. Five first-level grids with different scales from 270 to 990 m were established to calculate the area proportion of LCZ. The area proportion of LCZ was then applied in the stepwise regression model to quantitatively analyze its magnitude and direction of impact on the LST. The results suggest that the LCZ types of the study area with the highest and lowest average LST were LCZ2 (compact middle-rise building, 39.82°C) and LCZG (water body, 34.24°C), respectively. However, on most scales, the warming effect of LCZ2 was lower than that of LCZE (bare rock or paver), and the cooling effect of LCZG was lower than that of LCZD (low plants). The optimum results were obtained at a scale of 810 m. At this scale, the warming effect was in the order: LCZE (0.314) > LCZ2 (0.236) > LCZ3 (compact low-rise building, 0.135) > LCZ5 (open middle-rise, 0.084) > LCZ6 (open low-rise, 0.056); the cooling effect was in the order: LCZD (−0.272) > LCZA (dense trees, −0.104) > LCZG (−0.103). These findings can help to elucidate the unique warming and cooling effects of LCZ on the interaction condition and the construction of an urban human settlement. |
first_indexed | 2024-04-11T06:43:01Z |
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issn | 2296-2565 |
language | English |
last_indexed | 2024-04-11T06:43:01Z |
publishDate | 2022-11-01 |
publisher | Frontiers Media S.A. |
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series | Frontiers in Public Health |
spelling | doaj.art-e3d46c7cb3324cb7953ac00e998198e72022-12-22T04:39:25ZengFrontiers Media S.A.Frontiers in Public Health2296-25652022-11-011010.3389/fpubh.2022.10721741072174Warming and cooling effects of local climate zones on urban thermal environmentRui Zhang0Jun Yang1Jun Yang2Jun Yang3Dongqi Sun4Xinyue Ma5Wenbo Yu6Xiangming Xiao7Jianhong (Cecilia) Xia8Urban Climate and Human Settlements Research' Lab, Jangho Architecture College, Northeastern University, Shenyang, ChinaUrban Climate and Human Settlements Research' Lab, Jangho Architecture College, Northeastern University, Shenyang, ChinaSchool of Humanities and Law, Northeastern University, Shenyang, ChinaHuman Settlements Research Center, Liaoning Normal University, Dalian, ChinaKey Laboratory of Regional Sustainable Development Modeling, Institute of Geographic Sciences and Natural Resources Research, CAS, Beijing, ChinaUrban Climate and Human Settlements Research' Lab, Jangho Architecture College, Northeastern University, Shenyang, ChinaSchool of Humanities and Law, Northeastern University, Shenyang, ChinaDepartment of Microbiology and Plant Biology, Center for Earth Observation and Modeling, University of Oklahoma, Norman, OK, United StatesSchool of Earth and Planetary Sciences (EPS), Curtin University, Perth, WA, AustraliaUnderstanding the thermal characteristics and contribution ranking of local climate zones (LCZs) is essential since they can help in maintaining environmental harmony. However, previous studies only considered independent effects and could not analyze the combined effects of LCZ on land surface temperature (LST). In this study, we propose a new method to establish an interaction model between LCZs. Five first-level grids with different scales from 270 to 990 m were established to calculate the area proportion of LCZ. The area proportion of LCZ was then applied in the stepwise regression model to quantitatively analyze its magnitude and direction of impact on the LST. The results suggest that the LCZ types of the study area with the highest and lowest average LST were LCZ2 (compact middle-rise building, 39.82°C) and LCZG (water body, 34.24°C), respectively. However, on most scales, the warming effect of LCZ2 was lower than that of LCZE (bare rock or paver), and the cooling effect of LCZG was lower than that of LCZD (low plants). The optimum results were obtained at a scale of 810 m. At this scale, the warming effect was in the order: LCZE (0.314) > LCZ2 (0.236) > LCZ3 (compact low-rise building, 0.135) > LCZ5 (open middle-rise, 0.084) > LCZ6 (open low-rise, 0.056); the cooling effect was in the order: LCZD (−0.272) > LCZA (dense trees, −0.104) > LCZG (−0.103). These findings can help to elucidate the unique warming and cooling effects of LCZ on the interaction condition and the construction of an urban human settlement.https://www.frontiersin.org/articles/10.3389/fpubh.2022.1072174/fullland surface temperaturelocal climate zonestepwise regression modelurban thermal characteristicsShenyang |
spellingShingle | Rui Zhang Jun Yang Jun Yang Jun Yang Dongqi Sun Xinyue Ma Wenbo Yu Xiangming Xiao Jianhong (Cecilia) Xia Warming and cooling effects of local climate zones on urban thermal environment Frontiers in Public Health land surface temperature local climate zone stepwise regression model urban thermal characteristics Shenyang |
title | Warming and cooling effects of local climate zones on urban thermal environment |
title_full | Warming and cooling effects of local climate zones on urban thermal environment |
title_fullStr | Warming and cooling effects of local climate zones on urban thermal environment |
title_full_unstemmed | Warming and cooling effects of local climate zones on urban thermal environment |
title_short | Warming and cooling effects of local climate zones on urban thermal environment |
title_sort | warming and cooling effects of local climate zones on urban thermal environment |
topic | land surface temperature local climate zone stepwise regression model urban thermal characteristics Shenyang |
url | https://www.frontiersin.org/articles/10.3389/fpubh.2022.1072174/full |
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