对“近表层洋流和温度剖面短时演变的简单模式”评论的答复
Reply to comment on `A simple model for the short-time evolution of near-surface current and temperature profiles'
摘要：
这是我们对Walter Eifler就我们的论文“近表层洋流和温度分布图短期演变的简单模型”（arXiv：physics/0503186，已接受在《深海研究II》上发表）发表的评论的答复。虽然Eifler提出了真正的问题，我们的模型的有效性和适用性，但我们仍然认为，它是有价值的短期演变的上层海洋剖面的电流和温度。在稳定的风应力作用下，有效涡粘滞性在无限长时间内趋于无穷大，这一事实并不奇怪。它可以解释为一个垂直移动的涡粘滞性剖面和增加的主要湍流涡的大小在假设条件下的小分层和无限水深。
英文摘要：
This is our response to a comment by Walter Eifler on our paper `A simple model for the short-time evolution of near-surface current and temperature profiles' (arXiv:physics/0503186, accepted for publication in Deep-Sea Research II). Although Eifler raises genuine issues regarding our model's validity and applicability, we are nevertheless of the opinion that it is of value for the short-term evolution of the upper-ocean profiles of current and temperature. The fact that the effective eddy viscosity tends to infinity for infinite time under a steady wind stress may not be surprising. It can be interpreted as a vertical shift of the eddy viscosity profile and an increase in the size of the dominant turbulent eddies under the assumed conditions of small stratification and infinite water depth.
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