Importance of radiative transfer processes in urban climate models: a study based on the PALM 6.0 model system

被引:24
作者
Salim, Mohamed H. [1 ,2 ]
Schubert, Sebastian [1 ]
Resler, Jaroslav [3 ]
Krc, Pavel [3 ]
Maronga, Bjorn [4 ,5 ]
Kanani-Suehring, Farah [4 ,6 ]
Suehring, Matthias [4 ]
Schneider, Christoph [1 ]
机构
[1] Humboldt Univ, Geog Dept, Berlin, Germany
[2] Aswan Univ, Fac Energy Engn, Aswan, Egypt
[3] Czech Acad Sci, Inst Comp Sci, Prague, Czech Republic
[4] Leibniz Univ Hannover, Inst Meteorol & Climatol, Hannover, Germany
[5] Univ Bergen, Geophys Inst, Bergen, Norway
[6] Harz Energie GmbH & Co KG, Goslar, Germany
关键词
LARGE-EDDY SIMULATION; SOLAR-RADIATION; WIND FLOW; AIR-FLOW; IMPACT; BALANCE; TEMPERATURE; SENSITIVITY; VALIDATION; DISPERSION;
D O I
10.5194/gmd-15-145-2022
中图分类号
P [天文学、地球科学];
学科分类号
07 ;
摘要
Including radiative transfer processes within the urban canopy layer into microscale urban climate models (UCMs) is essential to obtain realistic model results. These processes include the interaction of buildings and vegetation with shortwave and longwave radiation, thermal emission, and radiation reflections. They contribute differently to the radiation budget of urban surfaces. Each process requires different computational resources and physical data for the urban elements. This study investigates how much detail modellers should include to parameterize radiative transfer in microscale building-resolving UCMs. To that end, we introduce a stepwise parameterization method to the Parallelized Large-eddy Simulation Model (PALM) system 6.0 to quantify individually the effects of the main radiative transfer processes on the radiation budget and on the flow field. We quantify numerical simulations of both simple and realistic urban configurations to identify the major and the minor effects of radiative transfer processes on the radiation budget. The study shows that processes such as surface and vegetation interaction with shortwave and longwave radiation will have major effects, while a process such as multiple reflections will have minor effects. The study also shows that radiative transfer processes within the canopy layer implicitly affect the incoming radiation since the radiative transfer model is coupled to the radiation model. The flow field changes considerably in response to the radiative transfer processes included in the model. The study identified those processes which are essentially needed to assure acceptable quality of the flow field. These processes are receiving radiation from atmosphere based on the sky-view factors, interaction of urban vegetation with radiation, radiative transfer among urban surfaces, and considering at least single reflection of radiation. Omitting any of these processes may lead to high uncertainties in the model results.
引用
收藏
页码:145 / 171
页数:27
相关论文
共 52 条
[1]   Analysis of airflow over building arrays for assessment of urban wind environment [J].
Abd Razak, Azli ;
Hagishima, Aya ;
Ikegaya, Naoki ;
Tanimoto, Jun .
BUILDING AND ENVIRONMENT, 2013, 59 :56-65
[2]  
[Anonymous], 1977, Methods in Computational Physics: Advances in Research and Applications, DOI [DOI 10.1016/B978-0-12-460817-7.50009-4, 10.1016/B978-0-12-460817-7.50009-4]
[3]  
Archambeau F., 2004, Int. J. Finite, V1
[4]   CFD modeling of the impact of solar radiation in a tridimensional urban canyon at different wind conditions [J].
Bottillo, S. ;
Vollaro, A. De Lieto ;
Galli, G. ;
Vallati, A. .
SOLAR ENERGY, 2014, 102 :212-222
[5]   Atmospheric radiative transfer modeling: a summary of the AER codes [J].
Clough, SA ;
Shephard, MW ;
Mlawer, E ;
Delamere, JS ;
Iacono, M ;
Cady-Pereira, K ;
Boukabara, S ;
Brown, PD .
JOURNAL OF QUANTITATIVE SPECTROSCOPY & RADIATIVE TRANSFER, 2005, 91 (02) :233-244
[6]   Evaluating the ENVI-met microscale model for suitability in analysis of targeted urban heat mitigation strategies [J].
Crank, Peter J. ;
Sailor, David J. ;
Ban-Weiss, George ;
Taleghani, Mohammad .
URBAN CLIMATE, 2018, 26 :188-197
[7]   The Common Land Model [J].
Dai, YJ ;
Zeng, XB ;
Dickinson, RE ;
Baker, I ;
Bonan, GB ;
Bosilovich, MG ;
Denning, AS ;
Dirmeyer, PA ;
Houser, PR ;
Niu, GY ;
Oleson, KW ;
Schlosser, CA ;
Yang, ZL .
BULLETIN OF THE AMERICAN METEOROLOGICAL SOCIETY, 2003, 84 (08) :1013-1023
[8]   Influence of Thermal Effects on the Wind Field Within the Urban Environment [J].
Dimitrova, R. ;
Sini, Jean-Francois ;
Richards, K. ;
Schatzmann, M. ;
Weeks, M. ;
Garcia, E. Perez ;
Borrego, C. .
BOUNDARY-LAYER METEOROLOGY, 2009, 131 (02) :223-243
[9]   The numerical flow model MISKAM: State of development and evaluation of the basic version [J].
Eichhorn, Joachim ;
Kniffka, Anke .
METEOROLOGISCHE ZEITSCHRIFT, 2010, 19 (01) :81-90