Evaporating waterbody effects in a simplified urban neighbourhood: A RANS analysis

被引:6
作者
Ampatzidis, Petros [1 ]
Cintolesi, Carlo [2 ]
Petronio, Andrea [3 ]
Di Sabatino, Silvana [2 ]
Kershaw, Tristan [1 ]
机构
[1] Univ Bath, Dept Architecture & Civil Engn, Bath BA2 7AY, Somerset, England
[2] Univ Bologna, Dept Phys & Astron, Via Irnerio 46, I-40126 Bologna, Italy
[3] IEFLUIDS Srl, Piazzale Europa 1, I-34127 Trieste, Italy
基金
英国工程与自然科学研究理事会;
关键词
Urbanwaterbody; Bluespace; Nature-basedsolutions; Evaporation; CFD; RANS; OpenFOAM; LARGE-EDDY SIMULATION; PEDESTRIAN WIND ENVIRONMENT; ATMOSPHERIC BOUNDARY-LAYER; THIN-FILM EVAPORATION; HEAT-ISLAND; CFD SIMULATION; GREEN INFRASTRUCTURE; THERMAL ENVIRONMENT; COOPERATIVE PROJECT; WALL FUNCTION;
D O I
10.1016/j.jweia.2022.105078
中图分类号
TU [建筑科学];
学科分类号
0813 ;
摘要
The incorporation of nature-based solutions comprising green and blue infrastructure is often touted as a way to cool cities and enhance pollutant removal. However, there is little agreement between different methodologies to measure the effect of any single intervention. Here, we present 3D steady RANS simulations to investigate the influence of waterbody on in-canyon flow structure, temperature (T*) and water vapour (!*) distribution in a simplified urban neighbourhood. A novel solver that captures evaporation effects is developed and validated against wind tunnel experiments. Simulations are performed under neutral atmospheric conditions for forced -and mixed-convection cases and different air-water temperature differences, indicative of either daytime or night-time conditions. Results under forced convection show minimal impact on the flow structure, whilst T* and !* effects are distributed primarily over and around the water surface. However, the mixed-convection case shows that a cooler waterbody weakens the principal vortex in the open square, whilst T* and !* effects reach further upwind and are more widely distributed in the spanwise direction. A warmer waterbody is shown to disrupt the skimming flow structure, indicating a possible heat and pollutant removal mechanism from around the waterbody and also downwind canyons.
引用
收藏
页数:20
相关论文
共 103 条
[41]   Passive scalar diffusion in and above urban-like roughness under weakly stable and unstable thermal stratification conditions [J].
Kanda, Isao ;
Yamao, Yukio .
JOURNAL OF WIND ENGINEERING AND INDUSTRIAL AERODYNAMICS, 2016, 148 :18-33
[42]   Roughness lengths for momentum and heat derived from outdoor urban scale models [J].
Kanda, M. ;
Kanega, M. ;
Kawai, T. ;
Moriwaki, R. ;
Sugawara, H. .
JOURNAL OF APPLIED METEOROLOGY AND CLIMATOLOGY, 2007, 46 (07) :1067-1079
[43]  
Kato T., 2009, P HYDRAULIC ENG JAPA, V53, P343
[44]  
Kim JJ, 1999, J APPL METEOROL, V38, P1249, DOI 10.1175/1520-0450(1999)038<1249:ANSOTE>2.0.CO
[45]  
2
[46]   Physical experiments to investigate the effects of street bottom heating and inflow turbulence on urban street-canyon flow [J].
Kim, JJ ;
Baik, JJ .
ADVANCES IN ATMOSPHERIC SCIENCES, 2005, 22 (02) :230-237
[47]   Assessment of thermally comfortable urban spaces in Amsterdam during hot summer days [J].
Klok, Lisette ;
Rood, Niek ;
Kluck, Jeroen ;
Kleerekoper, Laura .
INTERNATIONAL JOURNAL OF BIOMETEOROLOGY, 2019, 63 (02) :129-141
[48]   Evaluating the cooling effects of green infrastructure: A systematic review of methods, indicators and data sources [J].
Koc, Carlos Bartesaghi ;
Osmond, Paul ;
Peters, Alan .
SOLAR ENERGY, 2018, 166 :486-508
[49]  
Kovar-Panskus A, 2002, URBAN AIR QUALITY - RECENT ADVANCES, PROCEEDINGS, P555
[50]  
Launder B. E., 1974, Computer Methods in Applied Mechanics and Engineering, V3, P269, DOI 10.1016/0045-7825(74)90029-2