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The bottom Ekman layer and the apparent violation of the maximum principle

机译:Ekman底层和明显违反最大原则

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摘要

The solution for the bottom Ekman layer has a somewhat counter intuitive character, which seems to violate the maximum principle: at a certain level the velocity within the Ekman layer is higher than the velocity in the geostrophic layer above. I explain this character by looking at an analogous problem in an inertial frame of reference and show that it is the result of observing the flow from a rotating frame of reference (i.e. within a system that is not in steady state). The flow in the bottom Ekman layer is a superposition of the flow that results from the force exerted on the fluid by the rotating Earth and of the flow that results from the pressure-gradient term. Therefore, at a certain level the speed is higher than the speed of the geostrophic layer above which results from the pressure gradient alone.
机译:底部埃克曼层的解决方案具有某种相反的直觉特性,这似乎违反了最大原则:在一定水平上,埃克曼层内的速度高于上方地转层的速度。我通过查看惯性参考系中的一个类似问题来解释此特性,并表明它是观察来自旋转参考系(即在非稳态系统中)的流量的结果。底部埃克曼层中的流动是由旋转的地球施加在流体上的力引起的流动与由压力梯度项产生的流动的叠加。因此,在一定水平上,该速度高于地转层的速度,在该速度以上,地转层的速度仅由压力梯度引起。

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