多辐射层和对流层旋转倾斜f面中的穿透对流

Sethulakshmy Edathara Sreenivasan and Tao Cai
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引用次数: 0

摘要

在本文中,我们对具有多个对流稳定层和不稳定层的旋转倾斜f平面中的穿透对流进行了线性不稳定性分析。我们的研究结果表明,穿透距离随着旋转和分层强度的增加而减小。我们还观察到,先前在两层模型中确定的远对流、多卷对流和切断对流在多层模型中也存在。对于三层模型,在两极处穿透对流表现为上下对称的流动模式。然而,当气流向赤道或极地方向漂移时,这种对称在倾斜的f面中被破坏。在中低纬度地区,向极地的气流有利于上层的穿透,而向赤道的气流有利于下层的穿透。当振荡对流发生时,在多层模型中也观察到上下对称的破坏。我们的发现表明,在多层结构的恒星或行星上,向上和向下的穿透可能有很大的不同。而在较强的稳定成分梯度作用下,不稳定性有所降低。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Penetrative Convection in Rotating Tilted f-plane with Multiple Radiative and Convective Layers
In this paper, we conducted a linear instability analysis to investigate penetrative convection in rotating, tilted f-planes with multiple convectively stable and unstable layers. Our findings indicate that penetrative distance decreases with increasing rotational and stratification strengths. We also observed that teleconvection, multiroll convection, and cutoff convection, previously identified in two-layer models, are present in multilayer models. For a three-layer model, the flow exhibits an up-down symmetric pattern for penetrative convection at the poles. However, this symmetry is disrupted in tilted f-planes when the flow drifts in equatorward or poleward directions. At mid- to low latitudes, poleward flow tends to enhance penetration in the upper layers, while equatorward flow facilitates penetration in the lower layers. The disruption of up-down symmetry is also observed in multilayer models with more layers when oscillatory convection occurs. Our findings suggest that upward and downward penetration could be significantly different in stars or planets with multilayer structures. However, under a strong stable composition gradient, the instability is found to be reduced.
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