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<p>open ice-free liquid surface area of the lake shrinks. This reduces fetch distances. Secondly, the water temperature nears freezing, reducing overall latent heat energy available to produce squalls. To end the production of lake-effect precipitation, a complete freeze is often not necessary.</p>

<p>Even when precipitation is not produced, cold air passing over warmer water may produce cloud cover. Fast-moving mid-latitude cyclones, known as <a href="page.php?w=Alberta_clipper">Alberta clipper</a>s, often cross the Great Lakes. After the passage</p><p>
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