城市峡谷能量收支模拟[j]。模型结构及灵敏度试验

Gerald M. Mills
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引用次数: 65

摘要

本文介绍了一个用于模拟城市峡谷气候的简单数值模型的公式和结果。该模型本质上是二维的,它是基于这样的观察:穿过对称峡谷长轴的环境气流在峡谷空气空间内驱动一个循环涡,从而导致峡谷顶部的热量、质量和动量交换。描述了一个简单的模型,该模型由两个部分组成:一个是峡谷内气流与环境风速的半经验模型,另一个是峡谷表面的能量收支模型。该模式能够模拟峡谷气候的许多方面,包括峡谷表面和顶部的能量收支以及地表和空气温度。模型的敏感性试验表明,峡谷顶部能量收支对峡谷参数的许多变化具有显著的稳定性。峡谷的几何形状(以高/宽比表示)引起了最大的变化,狭窄程度的增加与峡谷顶部的热交换减少有关。该模型的预测直观合理,与现有的测量数据比较良好。结果表明,城市边界与冠层在热交换方面的耦合可能是峡谷几何形状的函数。
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Simulation of the energy budget of an urban canyon—I. Model structure and sensitivity test

This paper presents the formulation and results of a simple numerical model designed to simulate the climate of an urban canyon. The model is two-dimensional in nature and is based on the observation that ambient airflow which tranverses the long-axis of a symmetrical canyon drives a circulating vortex within the canyon air space which results in the exchange of heat, mass and momentum at the canyon top. A simple model is described which consists of two components: a semi-empirical model to relate within-canyon airflow to ambient wind velocity, and an energy budget model for canyon surfaces. The model is capable of simulating many aspects of the canyon climate, including the canyon surface and top energy budget and surface and air temperatures. Sensitivity tests with the model indicate that the canyon top energy budget is remarkably stable for many changes in canyon parameters. Canyon geometry (expressed as a height/width ratio) caused the greatest changes with increased narrowness being associated with less heat exchange across the canyon top. The model's predictions appear intuitively reasonable and compare well with existing measurement data. The results suggest that the coupling between the urban boundary and canopy layers in terms of heat exchange may be a function of canyon geometry.

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