Parallel rows of clouds can stretch for hundreds of kilometers over the open ocean.
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Cool air moving across Arctic sea ice gives rise to long parallel bands of cumulus clouds over the Norwegian Sea.
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Cold winds blowing over the sea helped form rows of cumulus clouds.
Image of the Day Atmosphere Water Unique Imagery Snow and Ice
Cold air blows over warmer water to produce thin, parallel lines of clouds.
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Most of us prefer our winter roads free of ice, but some cloud formations depend on it.
Cool air blowing southward across the sea ice and over the comparatively warmer open water produced long, parallel bands of cumulus clouds.
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The Sea of Okhotsk is a winter ice factory and a year-round cloud factory.
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Cold and dry air from Siberia typically produce this cloud formation over the sea from November through January.
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Cloud streets form thousands of feet above the Earth’s surface.
Tucked between Siberia and Russia's frozen Kamchatka Peninsula, the Sea of Okhotsk was a field of ice in February 2007.
An uncommon display of cloud streets formed off of the northern coast of Australia.
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Cold air moving over relatively warm ocean water produced a pattern of clouds that lined up in organized rows.
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Distinctive lines of clouds that mirror the shape of the shore hang over the Aral Sea in this photo-like image.
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The Aqua satellite captured this image of cloud streets over the Black Sea in January 2015.
Atmosphere Unique Imagery
Cold air blowing between warmer water and warm upper-level air masses can produce long lines of cumulus clouds.
Dry air surging off the western coast of Africa ran into a wall of moist air over the Atlantic, creating a distinctive line in a marine cloud layer.
Like the freshly raked white sand of a well-tended Japanese garden, rows of clouds stream over the Bering Sea from the edge of the sea ice.
The MODIS instrument on NASA’s Terra satellite collected this natural-color view of cloud streets over the ocean off of New England and the Canadian Maritimes on January 24, 2011.
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Impressive thunderclouds run along the spine of the Indonesian island of Flores, a result of ocean breezes and steep mountains.
Sea breezes and differential heating fill the afternoon sky with puffs of white clouds.
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