Steady Convective Motion in a Horizontal Layer of Fluid Heated Uniformly from Above and Cooled Non‐uniformly from Below
Steady Convective Motion in a Horizontal Layer of Fluid Heated Uniformly from Above and Cooled Non‐uniformly from Below
复制标题
从上方均匀加热、从下方非均匀冷却的水平流体层中的稳定对流运动
DOI：
10.1111/j.2153-3490.1957.tb01896.x
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发表时间：
1957
期刊：
影响因子：
2
通讯作者：
G. Veronis
中科院分区：
文献类型：
--
作者：
H. Stommel;G. Veronis
重力稳定的流体层在底部（或顶部）被不均匀（正弦）加热，并建立热对流状态。针对以下情况制定了示例：(i) 没有旋转，(ii) 均匀旋转，以及 (iii) 不均匀旋转（β 平面）。 DOI：10.1111/j.2153-3490.1957.tb01896.x
A gravitationally stable fluid layer is heated non-uniformly (sinusoidally) at the bottom (or top) and a thermal convection regime is established. Examples are worked out for cases (i) without rotation (ii) with uniform rotation, and (iii) with non-uniform rotation (beta-plane). DOI: 10.1111/j.2153-3490.1957.tb01896.x