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Flow over Heated Terrain. Part Ⅰ: Linear Theory and Idealized Numerical Simulations

机译:流过加热的地形。第一部分:线性理论和理想的数值模拟

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The flow past heated topography is examined with both linear and nonlinear models. It is first shown that the forcing of an obstacle with horizontally homogenous surface heating can be approximated by the forcing of an obstacle with surface heating isolated over the obstacle. The small-amplitude flow past an obstacle with isolated heating is then examined with a linear model. Under the linear approximation, the flow response to heated topography is simply the addition of the separate responses to thermal and orographic forcing. These separate responses are first considered individually and then the combined response is examined. Nondimensional parameters are developed that measure the relative importance of thermal and orographic forcing. Nonaxisymmetric forcing is then considered by examining the flow along and across a heated elliptically shaped obstacle. It is shown that the low-level lifting is maximized when the flow is along the major axis of the obstacle. The linear solutions are then tested in a nonlinear anelastic model. The response to a heat source and orography are first examined separately. Good agreement is found between nonlinear and linear models for the individual responses to thermal and orographic forcing. The case of uniformly heated flow past an obstacle is then examined. In these simulations, the thermal response is isolated by subtracting the oro-graphic-only response from the full thermal-orographic response. The numerical simulations are able to capture the main features of the thermal response. Finally, numerical simulations of the flow along and across an elliptically shaped heated obstacle are examined, where it is verified that the lifting is maximized when the flow is along the major axis of the obstacle. These results are extended in Part Ⅱ of this study to examine the moist convective response to flow over both idealized terrain and the complex terrain of the Rocky Mountains of the United States.
机译:通过线性和非线性模型都可以检查经过加热地形的流量。首先表明,在水平均匀加热的情况下,对障碍物的强迫可以通过在障碍物上进行表面加热的情况下对障碍物的强迫来近似。然后使用线性模型检查经过隔离加热的障碍物的小振幅流。在线性近似下,对加热地形的流动响应只是将对热和地形强迫的独立响应相加。首先分别考虑这些单独的响应,然后检查组合响应。开发了无量纲参数,用于测量热强迫和地形强迫的相对重要性。然后,通过检查沿加热的椭圆形障碍物的流动并通过流动,来考虑非轴对称的作用力。结果表明,当水流沿着障碍物的长轴方向时,低空升力最大。然后在非线性弹性模型中测试线性解。首先分别检查对热源和地形的响应。在非线性模型和线性模型之间,对于热和地形强迫的个体响应之间找到了很好的一致性。然后检查均匀加热流过障碍物的情况。在这些模拟中,通过从整个热地形响应中减去仅纯正向图形响应来隔离热响应。数值模拟能够捕获热响应的主要特征。最后,检查了沿椭圆形加热障碍物的流动的数值模拟,并验证了当流体沿障碍物的主轴移动时提升力最大。这些结果在本研究的第二部分中得到了扩展,以检验美国落基山脉的理想对流和复杂对流的湿对流响应。

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