
Altostratus
© Frank Le Blancq WMO
Altostratus (lat. altus = high, stratus = spread out) is a gray or bluish-gray layer cloud that covers the sky extensively and often uniformly. It is thin enough to let the sun shine through like frosted glass, without any halo phenomena occurring. Altostratus consists of a mixture of water droplets and ice crystals and frequently extends over hundreds of kilometers. The cloud typically forms through large-scale, slow gliding of warm, moist air over a cold air mass, as occurs at warm fronts. As it thickens, altostratus can completely obscure the sun and transition into nimbostratus.
Highlighted: all species that occur with Altostratus.
Altostratus is one of the most important harbingers of an approaching warm front and typically signals precipitation within the next 6 to 24 hours. It characteristically forms as the successor to cirrostratus in the classic frontal sequence, gradually thickening into nimbostratus with sustained precipitation. Light rain or snow can already fall from thicker altostratus and reach the ground. In combination with falling air pressure, altostratus is a reliable indicator of impending deteriorating weather. However, isolated, thin altostratus can also dissipate without any subsequent precipitation.