Spatial differentiation of urban wind and thermal environment in different grid sizes

被引:124
作者
Yang, Jun [1 ,2 ]
Wang, Yichen [1 ]
Xiao, Xiangming [3 ,4 ]
Jin, Cui [1 ]
Xia, Jianhong [5 ]
Li, Xueming [1 ]
机构
[1] Liaoning Normal Univ, Human Settlements Res Ctr, Dalian 116029, Peoples R China
[2] Northeastern Univ, Jangho Architecture Coll, Shenyang 110169, Liaoning, Peoples R China
[3] Univ Oklahoma, Ctr Spatial Anal, Dept Microbiol & Plant Biol, Norman, OK 73019 USA
[4] Fudan Univ, Key Lab Biodivers Sci & Ecol Engn, Inst Biodivers Sci, Minist Educ, Shanghai 200433, Peoples R China
[5] Curtin Univ, Sch Earth & Planetary Sci, Perth, WA 65630, Australia
基金
中国国家自然科学基金;
关键词
Frontal area index; Urban thermal environment; Grid size; Maximum mutual information; Dalian city; LAND-SURFACE TEMPERATURE; HEAT-ISLAND; VENTILATION PATHS; AIR-TEMPERATURE; ROUGHNESS; PATTERN; IMPACT; AREAS; MODEL; SIMULATION;
D O I
10.1016/j.uclim.2019.100458
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
Due to rapid urbanization, China's urban morphology has undergone tremendous changes, resulting in an increased urban heat island (UHI) effect and negative impact of thermal environment, especially in summer. Studying the scale effect between urban wind and thermal environment can provide the best scale for the wind environment planning on mitigating UHI effect. Taking Dalian as an example, using multi-source data, a nonlinear correlation analysis was used to analyze the correlation between the frontal area index (FAI) and land 77uuyyhsurface temperature (LST) under different grids. The results show that first, FAI is sensitive to grid-size changes. When the grid size increases from 25 x 25m to 150 x 150m with a step size of 25 m, in July, the numbers of grids with FAI > 1 are 19,992, 1538, 153, 20, 4, and 0 (0%) accounting for 2.106%, 0.645%, 0.081%, 0.019%, 0.006%, and 0% of the total, respectively. In September, the numbers of grids with FAI > 1 are 17,633, 1643, 164, 22, 8, and 0, accounting for 1.849%, 0.689%, 0.155%, 0.037%, 0.021%, and 0% of the total, respectively. When the grid size is greater than or equal to 150 x 150 m, there is no grid with FAI > 1. Second, the most effective grid size to study the relationship between FAI and LST is 25 m. When the grid size increases from 25m to 300m with a step size of 25 m, the correlation between FAI and LST shows a significant decrease. When the grid size is 25 m, the correlation is the strongest.
引用
收藏
页数:13
相关论文
共 69 条
[1]   Coupled CFD and building energy simulations for studying the impacts of building height topology and buoyancy on local urban microclimates [J].
Allegrini, Jonas ;
Carmeliet, Jan .
URBAN CLIMATE, 2017, 21 :278-305
[2]   Urban roughness mapping validation techniques and some first results [J].
Bottema, M ;
Mestayer, PG .
JOURNAL OF WIND ENGINEERING AND INDUSTRIAL AERODYNAMICS, 1998, 74-6 :163-173
[3]   A WIND-TUNNEL STUDY OF AIR-FLOW IN WAVING WHEAT - SINGLE-POINT VELOCITY STATISTICS [J].
BRUNET, Y ;
FINNIGAN, JJ ;
RAUPACH, MR .
BOUNDARY-LAYER METEOROLOGY, 1994, 70 (1-2) :95-132
[4]  
Bureau of Urban Planning Dalian China, 2004, DAL CIT PLANN ARCH D
[5]   Assessing the resilience of urban areas to traffic-related air pollution: Application in Greater Paris [J].
Cariolet, Jean-Marie ;
Colombert, Morgane ;
Vuillet, Marc ;
Diab, Youssef .
SCIENCE OF THE TOTAL ENVIRONMENT, 2018, 615 :588-596
[6]   Pulling Vs. Pushing: Effect of Climatic Factors on Periodical Fluctuation of Russian and South Korean Tourist Demand in Hainan Island, China [J].
Chen, Fan ;
Liu, Jun ;
Ge, Quansheng .
CHINESE GEOGRAPHICAL SCIENCE, 2017, 27 (04) :648-659
[7]   A quantitative method to detect the ventilation paths in a mountainous urban city for urban planning: A case study in Guizhou, China [J].
Chen, Shi Ling ;
Lu, Jun ;
Yu, Wei Wei .
INDOOR AND BUILT ENVIRONMENT, 2017, 26 (03) :422-437
[8]   A simple approach for the development of urban climatic maps based on the urban characteristics in Tainan, Taiwan [J].
Chen, Yu-Cheng ;
Lin, Tzu-Ping ;
Lin, Chien-Ting .
INTERNATIONAL JOURNAL OF BIOMETEOROLOGY, 2017, 61 (06) :1029-1041
[9]  
CLARKE J F, 1971, International Journal of Biometeorology, V15, P41, DOI 10.1007/BF01804717
[10]  
Deyong H., 2015, Nat. Remote Sens. Bull., V19, P964, DOI [DOI 10.11834/JRS.20155038, 10.11834/jrs.20155038]