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首页> 外文期刊>International Journal of Climatology: A Journal of the Royal Meteorological Society >Simulating air temperature in an urban street canyon in all weather conditions using measured data at a reference meteorological station
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Simulating air temperature in an urban street canyon in all weather conditions using measured data at a reference meteorological station

机译:使用参考气象站的测量数据在所有天气条件下模拟城市街道峡谷中的气温

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摘要

A model is proposed that adapts data from a standard meteorological station to provide realistic site-specific air temperature in a city street exposed to the same meso-scale environment. In addition to a rudimentary description of the two sites, the canyon air temperature (CAT) model requires only inputs measured at standard weather stations; yet it is capable of accurately predicting the evolution of air temperature in all weather conditions for extended periods. It simulates the effect of urban geometry on radiant exchange; the effect of moisture availability on latent heat flux; energy stored in the ground and in building surfaces; air flow in the street based on wind above roof height; and the sensible heat flux from individual surfaces and from the street canyon as a whole. The CAT model has been tested on field data measured in a monitoring program carried out in Adelaide, Australia, in 2000-2001. After calibrating the model, predicted air temperature correlated well with measured data in all weather conditions over extended periods. The experimental validation provides additional evidence in support of a number of parameterisation schemes incorporated in the model to account for sensible heat and storage flux. Copyright (C) 2006 Royal Meteorological Society.
机译:提出了一种模型,该模型可以适应来自标准气象站的数据,以在暴露于相同中尺度环境的城市街道中提供实际的特定于站点的气温。除了对这两个站点的基本描述之外,峡谷空气温度(CAT)模型只需要在标准气象站测量的输入即可;但是它能够准确地预测所有天气条件下长时间的气温变化。它模拟了城市几何形状对辐射交换的影响;水分供应对潜热通量的影响;储存在地面和建筑物表面的能量;街道上的空气流动是基于屋顶高度以上的风;以及来自各个表面和整个街道峡谷的显热通量。 CAT模型已根据2000-2001年在澳大利亚阿德莱德进行的监测计划中测得的现场数据进行了测试。校准模型后,预测的气温与长时间内所有天气条件下的实测数据均具有良好的相关性。实验验证提供了额外的证据来支持模型中纳入的大量参数化方案,以说明显热和储热通量。版权所有(C)2006皇家气象学会。

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