Simulations of Nonhomogeneous Terrain Flows
Date Issued
2006
Date
2006
Author(s)
Shu, Jyh-Kwei
DOI
en-US
Abstract
微氣候中，大部分的地表層分析假定均勻地形流況和水平均勻流動。然而，一個均勻的環境系統在自然界中的存在是相當少見的。一個更有物理意義的有限體積法被用來考慮當流動受地表粗糙度影響時之變化。所以我們使用雷諾應力紊流模式，以了解大氣紊流結構如何被不同地表影響。
地表粗糙度對風速有相當深刻的影響。越粗糙的地表，則越易使大氣邊界層內的風速減速。此研究顯示從粗糙到平滑的紊流邊界層的變化小於平滑到粗糙。紊流強度的分佈也描述了邊界層的變化。地形變化越大則風速變化越大。
In microclimate, most surface layer analyses assume uniform terrain conditions and a horizontally-homogeneous flow. However, a homogeneous environmental system rarely exists in the nature. A finite volume method with more reasonable physical meanings is introduced to consider a flow field over a changed roughness surface. In order to know how various types of surface affect the atmospheric turbulence structure, RSM (Reynolds Stress Model) is used.
Surface roughness has a profound effect on wind speed. The rougher a terrain is, the more it retards the wind in the atmospheric boundary layer. This study reveals that the variation of turbulent boundary layer due to rough-to-smooth is less than that in the smooth-to-rough. The distribution of the turbulence intensities also depicts the variations of the internal boundary layer. The higher height a terrain surface has, the more variation it exhibit near the step change.
Subjects
雷諾應力紊流模式
非均勻地形
k-ε紊流模式
大氣邊界層
地表粗糙度
粗糙密度
Reynolds stress model
nonhomogeneous terrain
k-εmodel
Atmospheric boundary layer
surface roughness
roughness density
SDGs
Type
thesis
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