Stratus Clouds Cold Front at Lucy Brodie blog

Stratus Clouds Cold Front. Stratus clouds, in addition to being formed by radiative cooling of a moist clear layer, can be formed by lifting of moist air masses in. The classic cold front clouds produced along that steep, tall leading edge are cumulus, or “heaped,” clouds. As the cold front moves away, skies are mostly clear, but you might see either stratus or stratocumulus clouds. Stratus clouds usually emerge in stable atmospheric conditions, such as after the passage of a warm or occluded front, where the air is gently lifted over a cooler air mass.

Stratus cloud Alchetron, The Free Social Encyclopedia
from alchetron.com

Stratus clouds, in addition to being formed by radiative cooling of a moist clear layer, can be formed by lifting of moist air masses in. As the cold front moves away, skies are mostly clear, but you might see either stratus or stratocumulus clouds. Stratus clouds usually emerge in stable atmospheric conditions, such as after the passage of a warm or occluded front, where the air is gently lifted over a cooler air mass. The classic cold front clouds produced along that steep, tall leading edge are cumulus, or “heaped,” clouds.

Stratus cloud Alchetron, The Free Social Encyclopedia

Stratus Clouds Cold Front Stratus clouds usually emerge in stable atmospheric conditions, such as after the passage of a warm or occluded front, where the air is gently lifted over a cooler air mass. As the cold front moves away, skies are mostly clear, but you might see either stratus or stratocumulus clouds. The classic cold front clouds produced along that steep, tall leading edge are cumulus, or “heaped,” clouds. Stratus clouds, in addition to being formed by radiative cooling of a moist clear layer, can be formed by lifting of moist air masses in. Stratus clouds usually emerge in stable atmospheric conditions, such as after the passage of a warm or occluded front, where the air is gently lifted over a cooler air mass.

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