What is Altostratus?
A middle cloud type within the B family in the international cloud classification. These clouds consist of water droplets and sometimes ice crystals. In mid-latitudes, the cloud base varies between 15,000 and 20,000 feet. They can range in color from white to gray and bluish. Altostratus clouds can be fibrous or layered and may occasionally form a thick layer that obscures the sun and moon. The halo phenomenon is not observed with this cloud type. It is a good indicator of precipitation or a precursor to a storm. Virga-type clouds fall into this category. They are often formed by variations in low altostratus. They can cause light rain and snowfall. Subtypes of altostratus include opacus, precipitans, and translucidus.
Schedule a Demo Today
A new era is starting with fundamentally new forecasting with unprecedented precision!
Contact UsGlossary
A periodic cooling of sea surface temperatures in the central and eastern Pacific Ocean, often leading to altered global...
A periodic warming of sea surface temperatures in the central and eastern Pacific Ocean, significantly influencing global...
A bomb cyclone is a large mid-latitude storm that forms when a storm’s central pressure drops (i.e. “bombs out”), resulting...
CONQ is a meteorological abbreviation for significant convection observed in a specific area, often indicating unstable atmospheric...
Particles such as pollen, grass seeds, or dust in the air that cause allergies and are transported by winds.
A polar vortex is a circulating mass of air in the atmosphere, typically found in polar regions. This rotating air mass occurs...
A large body of air having similar horizontal temperature and moisture characteristics.
Meteorology is the scientific study of the atmosphere and weather processes. It involves observing, analyzing, and forecasting...
A weather watch means there is a risk of weather hazards in the near future, which could pose a threat to life/property....
The formation of fog when warm and moist air passes over a cool or cold surface or, conversely, when cold air passes over...

