the troposphere.
The moon does not have clouds like we see on Earth. It has an exosphere, which is a very thin layer of gases, including sodium and potassium, but these do not form clouds.
Clouds that form between 2000 m and 8000 m in altitude are typically altocumulus and altostratus clouds. Altocumulus clouds are fluffy and white with patches or layers, while altostratus clouds are gray or blue-gray and cover the sky with a veil-like layer.
Stratus clouds are often associated with drizzle. These low-level clouds form a uniform layer and are known for their ability to produce light precipitation like drizzle or light rain.
The name of the cloud that covers large areas and forms in layers is called a stratus cloud. Stratus clouds are low-level clouds that appear as a continuous layer with a fairly uniform gray color.
the troposphere.
The moon does not have clouds like we see on Earth. It has an exosphere, which is a very thin layer of gases, including sodium and potassium, but these do not form clouds.
stratus clouds. They are low-level clouds that appear in a continuous layer and bring overcast conditions. Stratus clouds can sometimes produce light precipitation.
Clouds and weather form in the troposphere, which is the lowest layer of the Earth's atmosphere. The troposphere extends from the Earth's surface up to an average altitude of about 7 to 17 kilometers (4 to 11 miles) depending on the location.
Stratus clouds typically form in the lowest layer of the atmosphere known as the troposphere. They are often seen at lower altitudes, usually below 6,500 feet, and can cover large areas of the sky with their flat, uniform appearance.
A form of clouds in which they are arranged in a horizontal band or layer. See Cloud.
Stratus clouds are typically associated with stable air. These clouds form in a layer and are often found in calm, stable weather conditions.
Stratus clouds are made of water droplets because they form at low altitudes where the air is cooler, causing water vapor to condense into liquid water droplets. These clouds appear as a uniform layer with a smooth, gray appearance due to the small size of the water droplets and the lack of vertical development.
Stratus clouds are uniform gray clouds that usually cover the entire sky. They can form when very weak, upward vertical air currents lift a thin layer of air high enough to initiate condensation. Stratus clouds also form when a layer of air is cooled from below to its dewpoint temperature and water vapor condenses into liquid droplets. Stratus clouds look like a layer of fog that never reaches the ground. In fact, fog that "lifts" off the ground forms a layer of low stratus clouds. Precipitation rarely falls from true stratus clouds since the upward vertical motion needed for precipitation is very weak, but light mist and drizzle can sometimes accompany stratus clouds.
Stratus clouds are typically associated with light rain and drizzle. These low-level clouds form a thick, gray layer that can produce steady, light precipitation over a large area.
no a stratus is a layer cloud.
Clouds that form between 2000 m and 8000 m in altitude are typically altocumulus and altostratus clouds. Altocumulus clouds are fluffy and white with patches or layers, while altostratus clouds are gray or blue-gray and cover the sky with a veil-like layer.