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<p><a href="page.php?w=cumulonimbus_cloud">cumulonimbus cloud</a>s producing thunderstorms commonly form along the front. <a href="page.php?w=Cumulonimbus_incus">Anvil</a> <a href="page.php?w=cirrus_cloud">cirrus cloud</a>s may spread a considerable distance downwind from the thunderstorms. The other cloud types associated with a cold front depend on atmospheric conditions such as airmass stability and wind shear. As the front approaches, middle-étage gives way to <a href="page.php?w=altostratus">altostratus</a> and low-level <a href="page.php?w=stratocumulus">stratocumulus</a></p><p>
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