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DOI | 10.1016/j.scitotenv.2018.10.025 |
Quantifying urban heat island intensity and its physical mechanism using WRF/UCM | |
Li, Huidong; Zhou, Yuyu; Wang, Xun; Zhou, Xu; Zhang, Huiwen; Sodoudi, Sahar | |
通讯作者 | Sodoudi, S (通讯作者) |
发表日期 | 2019 |
ISSN | 0048-9697 |
EISSN | 1879-1026 |
起始页码 | 3110 |
结束页码 | 3119 |
卷号 | 650 |
英文摘要 | Reliable quantification of urban heat island intensity (UHII) is crucial for the evaluation of extreme heat waves and the related heat stress. As a powerful approach for the study of urban climate, numericalmodels can simulate urban heat island (UHI) in both high spatial and temporal resolutions. However, accurate quantification of UHII using modelling grid data is still a challenge at present, due to the different criterions for the selection of urban/rural grids. This study simulates the high-resolution UHI in the city of Berlin using the Weather Research and Forecasting Model coupled with Urban Canopy Module. A new method to quantify UHII, which is based on the fitted linear functions of simulated 2-m air temperature (T-2m) using the impervious surface area inWRF grids (ISA(WRF)), was adopted and evaluated. The simulated T-2m matches the observations well, with a correlation coefficient of 0.95 (P < 0.01) and RMSE of 1.76 degrees C. The study area shows a strong UHI at nighttime. The simulated nighttime T-2m increases with the increase in the ISAWRF. The linear functions of simulated nighttime T-2m against ISAWRF are well fitted. The UHII is calculated as the products of the slopes of fitted functions and the largest ISAWRF. The derived UHII shows U-shaped diurnal variations, with high values at nighttime. The difference of simulated surface temperature and sensible heat flux between the impervious surface and the vegetation surface jointly determines the derived UHII. The large difference of surface temperature and the small difference of sensible heat flux between the impervious and the vegetation surface generate the high UHII at nighttime and vice versa during the daytime. The method of ISA(WRF)-based function of T-2m overcomes the problems of traditional methods in arbitrary selecting urban/rural grids. It can be used easily to quantify UHII and to do the comparison study of UHII between different cities. (c) 2018 Elsevier B.V. All rights reserved. |
关键词 | AIR-TEMPERATURECANOPY MODELWRF MODELCLIMATEIMPACTMODISSENSITIVITYSIMULATIONCONVECTIONINDICATORS |
英文关键词 | Urban heat island intensity; Impervious surface area; Urban parameters; WRF/UCM; Berlin |
语种 | 英语 |
WOS研究方向 | Environmental Sciences & Ecology |
WOS类目 | Environmental Sciences |
WOS记录号 | WOS:000447871400139 |
来源期刊 | SCIENCE OF THE TOTAL ENVIRONMENT
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来源机构 | 中国科学院青藏高原研究所 |
文献类型 | 期刊论文 |
条目标识符 | http://gcip.llas.ac.cn/handle/2XKMVOVA/259487 |
推荐引用方式 GB/T 7714 | Li, Huidong,Zhou, Yuyu,Wang, Xun,et al. Quantifying urban heat island intensity and its physical mechanism using WRF/UCM[J]. 中国科学院青藏高原研究所,2019,650. |
APA | Li, Huidong,Zhou, Yuyu,Wang, Xun,Zhou, Xu,Zhang, Huiwen,&Sodoudi, Sahar.(2019).Quantifying urban heat island intensity and its physical mechanism using WRF/UCM.SCIENCE OF THE TOTAL ENVIRONMENT,650. |
MLA | Li, Huidong,et al."Quantifying urban heat island intensity and its physical mechanism using WRF/UCM".SCIENCE OF THE TOTAL ENVIRONMENT 650(2019). |
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