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CONVECTIVE INSTABILITY IN AN INCLINED POROUS LAYER SUBJECT TO LINEARLY VARYING BOUNDARY TEMPERATURES

机译:倾斜的多孔层中的对流不稳定性受到线性变化的边界温度

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The stability of the parallel Hadley flow in an inclined plane porous layer where the boundaries are subject to a linearly varying temperature is studied. The inclination of the layer modifies the nature of the basic single-cell Hadley flow. In fact, the Hadley flow in an inclined layer displays a nonlinear velocity profile, with the possible existence of singularities for special inclination angles of the layer to the horizontal. The stability of the basic flow in the inclined porous layer is investigated by a linear analysis of the longitudinal rolls. The stability analysis provides the neutral stability curves for the onset of convection, and the critical values of the Rayleigh number for different inclinations of the layer. The linearized disturbance equations are solved by means of the collocation method of weighted residuals.
机译:研究了平行哈德利流动在倾斜平面多孔层中的稳定性,其中边界受到线性变化的温度。层的倾斜度改变了基本单细胞Hadley流的性质。实际上,倾斜层中的脊柱流动显示非线性速度曲线,其可能存在奇异性的奇点,用于层到水平的层的特殊倾斜角度。通过对纵向辊的线性分析来研究倾斜多孔层中基本流动的稳定性。稳定性分析提供了对流开始的中性稳定性曲线,以及用于层的不同倾斜的瑞利数的临界值。通过加权残留的搭配方法解决了线性化扰动方程。

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