sratus clouds and fog are generally found at the lowest altitude while I do not know where they are formed.
condensation level
Altitude affects the composition of clouds because the troposphere is very cold, so the clouds up higher are made of ice crystals. The clouds in the lower sections are made of water droplets or a mixture of water droplets and ice crystals.
The altitude where clouds form is called the condensation level or the lifting condensation level (LCL). It is the height at which air reaches its dew point temperature, causing water vapor to condense into visible water droplets, forming clouds.
Feet. Low clouds form at an altitude of 2000 feet.
Clouds are classified based on their appearance, altitude, and the processes that form them. The main types are cirrus (high-altitude, wispy clouds), cumulus (fluffy, white clouds typically associated with fair weather), and stratus (layered clouds that often cover the sky). Additionally, clouds can be categorized into low, middle, and high altitudes, with specific classifications such as nimbus (rain-bearing) and stratocumulus (low, lumpy clouds). This classification helps meteorologists predict weather patterns and understand atmospheric conditions.
Altitude
Three types of water found in the atmosphere are water vapor (gaseous form), liquid water in the form of clouds and precipitation, and ice crystals found in high-altitude clouds such as cirrus clouds.
Types of clouds that form in the lower atmosphere include cumulus clouds, stratus clouds, and stratocumulus clouds. These clouds typically indicate stable weather conditions and are found at lower altitudes.
Cirrocumulus clouds are very high altitude clouds that form in the troposphere. They form between 16,000 feet and 39,000 feet above the surface of the Earth.
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.
condensation level
Cirrus clouds are not likely to form below 2000 meters as they are high-altitude clouds found above 6000 meters. These clouds are wispy and thin, made up of ice crystals, and are often associated with fair weather.
The lowest clouds, known as surface fog or mist, can form right at ground level. These types of clouds essentially touch the Earth's surface.
Altitude affects the composition of clouds because the troposphere is very cold, so the clouds up higher are made of ice crystals. The clouds in the lower sections are made of water droplets or a mixture of water droplets and ice crystals.
Cirrus clouds are high-altitude clouds that form when strong winds blow the clouds into long, wispy streaks. These clouds are often feathery in appearance and indicate that turbulent weather may be approaching due to the high wind speeds at that altitude.
The altitude where clouds form is called the condensation level or the lifting condensation level (LCL). It is the height at which air reaches its dew point temperature, causing water vapor to condense into visible water droplets, forming clouds.
The highest clouds are polar mesospheric clouds, which, at heights from 76,000 to 85,000 m (altitude) are much higher than other types of clouds, such as cirrus and cumulonimbus. Cumulonimbus can exceptionally reach 23,000 m at the very top of a peaked formation, but these clouds normally form mainly within the 2,000 to 16,000 m range. Cirrus clouds, at a maximum height of about 18,000 m in tropical zones, are also much lower than polar mesosphericclouds.