In meteorology, an "'anticyclone "'( i . e . opposite to a cyclone ) is a weather stratocumulus or stratus cloud, colloquially known as " Anticylonic gloom ".
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CALIPSO has also been used in conjunction with the MODIS data to determine how aerosols within the planetary boundary layer might alter low planetary boundary layer stratus clouds.
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Being familiar with Wegener's earlier work, Bergeron theorized that ice crystals on the tree branches were scavenging vapor from the supercooled stratus cloud, preventing it from reaching the ground.
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One of its most striking features is the Chinook arch, which is a band of stationary stratus clouds caused by air rippling over the mountains due to orographic lifting.
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Warmer temperature in the eastern equatorial pacific increased water vapor greenhouse effect and reduced the area covered by highly reflective stratus clouds thus decreasing the albedo of the planet.
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The return flow of humid air into the Rio Grande Valley will produce a layer of stratus clouds along with patches of drizzle, which will migrate toward the southern Rockies.
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The low-altitude stratus clouds that make up the June Gloom cloud layer form over the nearby ocean, and are transported over the coastal areas by the region's prevailing westerly winds.
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In the wake of the low, residual moisture in the lowest few thousand feet of the atmosphere will cause low stratus clouds to linger over sections of eastern Minnesota and Iowa.
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Winds blowing up the gently sloping terrain towards the Rockies on the north side of this low will lead to showers, along with a nearly solid deck of low stratus clouds.
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A typical June Gloom morning consists of stratus clouds covering the coast of southern California, extending a varying distance inland depending on the strength of the June Gloom effect that day.
