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首页> 外文期刊>International Journal of Climatology: A Journal of the Royal Meteorological Society >Validation of a numerical model for urban energy-exchange using outdoor scale-model measurements
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Validation of a numerical model for urban energy-exchange using outdoor scale-model measurements

机译:使用室外比例模型测量结果验证城市能源交换的数值模型

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The objectives of our study are (1) to evaluate the simple urban energy balance model for mesoscale simulation (SUMM) using such data that are free from many real world uncertainties in respect to spatial variability in material, geometry, and land use, and (2) to analyse the sensitivity of land surface parameters (LSP), which are used in the model. The model was evaluated using the data obtained from comprehensive outdoor scale-model (COSMO) experiments during a period, which, covers roughly half of a year (winter and spring-early summer) including various wind conditions. SUMM simulated surface layer energy fluxes, surface temperature, and interior temperature fairly well under windy conditions while it underestimated sensible heat flux under calm conditions. On average, simulated sensible heat flux underestimated observed value by 30% (0.73 MJ m(-2) d(-1)) in daytime. Errors of net radiation (4%; 0.40 MJ m(-2) d(-1)) and heat storage (5%; 0.33 MJ m(-2) d(-1)) were smaller than that of sensible heat flux in daytime. This underestimation of sensible heat flux can be attributed to the inadequate parameterization of the surface layer bulk transfer coefficient used in SUMM under calm conditions. On the basis of the sensitivity analyses, parameterization of the surface layer bulk transfer coefficient using Monin-Obukhov similarity theory (MOST) shows that the model performance is very sensitive to this coefficient, while it is less sensitive to the relative Values of the bulk transfer coefficients of local faces. Copyright (c) 2007 Royal Meteorological Society.
机译:我们研究的目标是(1)使用此类数据评估中尺度模拟(SUMM)的简单城市能源平衡模型,这些数据在材料,几何形状和土地使用的空间变异性方面没有许多现实世界的不确定性,并且( 2)分析模型中使用的地表参数(LSP)的敏感性。该模型是使用一段时间内从综合室外比例模型(COSMO)实验获得的数据进行评估的,该过程涵盖大约半年的时间(冬季和春季初夏),包括各种风况。 SUMM在大风条件下相当好地模拟了表层能量通量,表面温度和内部温度,而在平静条件下低估了显热通量。平均而言,白天的模拟显热通量低估了观测值30%(0.73 MJ m(-2)d(-1))。净辐射(4%; 0.40 MJ m(-2)d(-1))和储热(5%; 0.33 MJ m(-2)d(-1))的误差小于显热通量白天。显热通量的这种低估可归因于在平静条件下SUMM中使用的表面层体积传递系数参数设置不充分。在敏感性分析的基础上,使用莫宁-奥布科夫相似理论(MOST)对表层整体转移系数进行参数化显示,模型性能对此系数非常敏感,而对整体转移的相对值则较不敏感局部面孔的系数。版权所有(c)2007皇家气象学会。

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