因此，最初引起兴趣大气波动系统和其他介质交界面所形成的波类似的东西不适宜作为进一步解释锋面的基础。

The initially attractive analogy between atmospheric wave systems and waves formed on interface of other media is, therefore, an insufficient-basis on which to develop explanations of frontal waves.

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当低压波沿着锋面移动时，云量的增长和稳定的雨量都是可以被预测的，偶尔还发大水。

When waves of low-pressure move along the front, cloudiness increases and steady rains can be expected, occasionally with flooding.

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