An analysis of microclimatic variation in a suburban environment

L.O. Myrup ∗, C.E. McGinn, R.G. Flocchini
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引用次数: 39

Abstract

An observational and modeling study of the microclimate of a suburban area, as related to the physical and biological nature of the site, is presented. The measurements and calculations are made in comparison with a nearby open agricultural location or “control site”. The measurement program was conducted during the summer of 1981 in Davis, CA, and consisted of a series of paired observations in which simultaneous measurements were made at a control site, located in a nearby rural area, and one suburban site at a time. Results indicate that this methodology was generally successful. The various suburban sites were as often cooler than the rural site as they were warmer. In one case, a suburban site was found to be substantially cooler, averaging 7.38°C over a 5 day period, than the rural site. This special case was observed to be associated with unusually dry environmental air resulting in large evaporative cooling in the plant canopy. Comparison between the suburban temperature deficit and the physical nature of the various sites reveals that canopy height explained most of the variance of this data set. Two generally important mechanisms are hypothesized to be operating in this system: the effect of canopy size on turbulent mixing and on site shading, especially of paved areas. A simple energy balance model was applied to study the processes that control the daytime suburban temperature deficit. In particular, it is found that suburban sites can be as cool as observed when the following conditions are obtained: low-canopy humidity, large canopy size, low wind speed and high radiation load. The model simulated the overall average suburban temperature deficit of all sites for physically reasonable choices of model parameters. It is pointed out that the fact that suburban areas may be cooler than surrounding rural areas may have significance to the problem of assessing the role of the urban heat island in relation to possible global warming.

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郊区环境小气候变化分析
本文介绍了一项与该地区的物理和生物性质有关的郊区小气候的观测和模拟研究。测量和计算是与附近的开放农业地点或“控制地点”进行比较。测量程序于1981年夏天在加利福尼亚州的戴维斯进行,由一系列成对观测组成,其中同时在位于附近农村地区的一个控制站点和一个郊区站点进行测量。结果表明,这种方法总体上是成功的。不同的郊区地点往往比农村地点更冷,也更温暖。在一个案例中,郊区站点被发现明显更冷,5天内平均温度为7.38°C,比农村站点低。这种特殊情况被观察到与异常干燥的环境空气有关,导致植物冠层的大量蒸发冷却。郊区温度差与各站点的物理性质比较表明,冠层高度解释了该数据集的大部分差异。假设在这个系统中有两个普遍重要的机制在起作用:冠层大小对湍流混合和场地遮阳的影响,特别是铺砌区域。应用一个简单的能量平衡模型研究了控制郊区白天温度亏缺的过程。特别是在满足低冠层湿度、大冠层尺寸、低风速和高辐射负荷的条件下,郊区站点可以像观测到的那样凉爽。为了合理选择模型参数,模型模拟了所有站点的总体平均城郊温度亏缺。有人指出,郊区可能比周围的农村地区更冷,这一事实可能对评估城市热岛与可能的全球变暖有关的作用的问题具有重要意义。
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