用流体静力数值模式模拟复杂地形上的风和空气污染

Fujio Kimura
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引用次数: 3

摘要

日本原子能研究所在位于日本东京北部的870米高的筑波山进行了扩散实验,并将静力风模型与网格型空气污染模型结合使用。该模型可以定性地模拟气流形态和浓度分布,包括在山上划分的羽流。尽管地形的水平尺度理论上并不比垂直尺度大,但计算的浓度结果与观测结果没有严重的差异。浓度分布对地表土壤温度非常敏感。这与环境风速和垂直温度分布同样重要。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
A simulation of wind and air pollution over complex terrain using a hydrostatic numerical model

A hydrostatic wind model used in conjunction with a grid-type air pollution model is applied to the diffusion experiments which were carried out by the Japan Atomic Energy Research Institute at Mt. Tsukuba, an 870 m mountain located to the north of Tokyo, Japan. The model can qualitatively simulate the flow pattern and concentration distribution, including divided plumes over the mountain. Even though the horizontal scale of the topography is theoretically not sufficiently larger than the vertical scale, the calculated concentration results are in no serious disagreement with those observed. The concentration distribution is quite sensitive to the surface soil temperature. This is as important as the ambient wind velocity and the vertical temperature profile.

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