The materials that make up noctilucent clouds are tiny water Ice crystals and dust particles.
It's kind of a zig zig. Look them up and you'll see.
Clouds can rise to various altitudes depending on their type and the atmospheric conditions. Generally, low clouds, like stratus and cumulus, form below 2,000 meters (6,600 feet), while mid-level clouds, such as altostratus and altocumulus, range from about 2,000 to 7,000 meters (6,600 to 23,000 feet). High clouds, like cirrus, can reach altitudes of 7,000 to 13,000 meters (23,000 to 42,000 feet) or even higher in some cases. The highest clouds, known as noctilucent clouds, can extend up to 85 kilometers (53 miles) in the upper atmosphere.
The mesosphere, located between the stratosphere and the thermosphere, does not contain specific "items" in the way we typically think of physical objects. Instead, it is characterized by various atmospheric phenomena such as temperature gradients, clouds known as noctilucent clouds, and meteors, which burn up upon entry into this layer. This region experiences decreasing temperatures with altitude, and it plays a crucial role in the Earth's atmospheric dynamics.
In the mesosphere, the most common occurrence is the formation of noctilucent clouds, which are thin and wispy clouds that form at high altitudes. Additionally, meteors burn up in the mesosphere, creating the phenomenon known as shooting stars. The mesosphere is also the coldest layer of Earth's atmosphere, with temperatures decreasing with altitude.
Light itself cannot destroy clouds. However, intense sunlight can increase evaporation, causing clouds to dissipate as the water droplets that make up the clouds turn into water vapor. Additionally, strong sunlight can also help to disperse clouds by breaking up their formation.
The mesosphere is the layer of the Earth's atmosphere that lies between the stratosphere and the thermosphere. It is characterized by its extreme cold temperatures and the presence of noctilucent clouds, which are the highest clouds in the atmosphere. The mesosphere is also where most meteorites burn up upon entering the Earth's atmosphere.
In the mesosphere, you can find various objects such as meteoroids, which are small rocky or metallic bodies that enter the Earth's atmosphere and burn up due to friction with the air. Additionally, the mesosphere is where you can find noctilucent clouds, which are thin, wispy clouds that form at high altitudes and are illuminated by the sun when it is below the horizon. The mesosphere also contains the ozone layer, which helps protect the Earth from harmful ultraviolet radiation.
It's kind of a zig zig. Look them up and you'll see.
The highest cloud type is called noctilucent clouds, which form in the mesosphere, about 50 miles above the Earth's surface. They are only visible during twilight and are made up of tiny ice crystals.
Clouds can rise to various altitudes depending on their type and the atmospheric conditions. Generally, low clouds, like stratus and cumulus, form below 2,000 meters (6,600 feet), while mid-level clouds, such as altostratus and altocumulus, range from about 2,000 to 7,000 meters (6,600 to 23,000 feet). High clouds, like cirrus, can reach altitudes of 7,000 to 13,000 meters (23,000 to 42,000 feet) or even higher in some cases. The highest clouds, known as noctilucent clouds, can extend up to 85 kilometers (53 miles) in the upper atmosphere.
A low level cloud is a cloud that forms below 6,500 feet (2,000 meters) in the atmosphere. These clouds are typically composed of water droplets and are often associated with precipitation. Examples of low level clouds include stratus clouds, cumulus clouds, and stratocumulus clouds.
Noctilucent clouds are the highest clouds in Earth's atmosphere, located in the mesosphere at altitudes of around 76 to 85 kilometres (47 to 53 mi). They are normally too faint to be seen, and are visible only when illuminated by sunlight from below the horizon while the lower layers of the atmosphere are in the Earth's shadow.
The mesosphere, located between the stratosphere and the thermosphere, does not contain specific "items" in the way we typically think of physical objects. Instead, it is characterized by various atmospheric phenomena such as temperature gradients, clouds known as noctilucent clouds, and meteors, which burn up upon entry into this layer. This region experiences decreasing temperatures with altitude, and it plays a crucial role in the Earth's atmospheric dynamics.
The mesosphere does not directly affect life on Earth as it is too high up in the atmosphere. It plays a role in protecting the Earth's surface by absorbing and dissipating the energy from incoming meteors, preventing them from reaching the surface. Additionally, the mesosphere is important for certain atmospheric phenomena like noctilucent clouds.
In the mesosphere, the most common occurrence is the formation of noctilucent clouds, which are thin and wispy clouds that form at high altitudes. Additionally, meteors burn up in the mesosphere, creating the phenomenon known as shooting stars. The mesosphere is also the coldest layer of Earth's atmosphere, with temperatures decreasing with altitude.
Light itself cannot destroy clouds. However, intense sunlight can increase evaporation, causing clouds to dissipate as the water droplets that make up the clouds turn into water vapor. Additionally, strong sunlight can also help to disperse clouds by breaking up their formation.
the water from the sea evaporates to the sky. when it goes higher up, it condenses to form water doplets. it would then gather together to make clouds.