Stratus Clouds Explanation. Often the scene of dull, overcast days in its 'nebulosus' form, they. They can produce an overcast day or light rain or snow. stratus clouds, in addition to being formed by radiative cooling of a moist clear layer, can be formed by lifting of moist. These stratus fractus clouds constitute a. Cirrus clouds are white wisps high in the sky. stratus clouds are sheets or layers of clouds. Nimbus clouds are either cumulus or stratus clouds that produce precipitation. stratus clouds are born from a simple process: They appear frequently in the mornings over mountainous areas. Rain and snow clouds tend to be gray rather than white. stratus clouds are low altitude clouds which form up to 800 meters (0.5 miles) above the ground. When the air reaches its dew point temperature, the invisible water vapor. As warm, moist air rises and encounters cooler air, it cools down. stratus is sometimes observed as more or less joined cloud fragments with varying luminance. This type of clouds does not produce halo phenomena except for some occasions at very low temperatures.
from astronimus.com
Often the scene of dull, overcast days in its 'nebulosus' form, they. stratus clouds are born from a simple process: stratus clouds are low altitude clouds which form up to 800 meters (0.5 miles) above the ground. They appear frequently in the mornings over mountainous areas. stratus is sometimes observed as more or less joined cloud fragments with varying luminance. Cirrus clouds are white wisps high in the sky. Rain and snow clouds tend to be gray rather than white. When the air reaches its dew point temperature, the invisible water vapor. These stratus fractus clouds constitute a. Nimbus clouds are either cumulus or stratus clouds that produce precipitation.
The Stratus Clouds AstronimUs
Stratus Clouds Explanation As warm, moist air rises and encounters cooler air, it cools down. They appear frequently in the mornings over mountainous areas. Cirrus clouds are white wisps high in the sky. This type of clouds does not produce halo phenomena except for some occasions at very low temperatures. When the air reaches its dew point temperature, the invisible water vapor. Nimbus clouds are either cumulus or stratus clouds that produce precipitation. stratus is sometimes observed as more or less joined cloud fragments with varying luminance. As warm, moist air rises and encounters cooler air, it cools down. These stratus fractus clouds constitute a. stratus clouds, in addition to being formed by radiative cooling of a moist clear layer, can be formed by lifting of moist. stratus clouds are low altitude clouds which form up to 800 meters (0.5 miles) above the ground. stratus clouds are born from a simple process: Often the scene of dull, overcast days in its 'nebulosus' form, they. They can produce an overcast day or light rain or snow. stratus clouds are sheets or layers of clouds. Rain and snow clouds tend to be gray rather than white.
