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The mesosphere is the third layer of Earth's atmosphere, situated above the stratosphere and below the thermosphere. It extends from about 50 kilometers (31 miles) to approximately 85 kilometers (53 miles) above sea level. The boundary between the mesosphere and the thermosphere is called the mesopause, which is the point where temperature begins to increase again due to the absorption of solar radiation in the thermosphere.
The mesosphere is the layer of Earth's atmosphere above the stratosphere and below the thermosphere. It extends from about 31 miles (50 kilometers) to 53 miles (85 kilometers) above the Earth's surface. The thickness of the mesosphere can vary due to factors such as temperature and atmospheric conditions, but on average it is about 22 miles (35 kilometers) thick.
The mesosphere extends from about 31 miles (50 kilometers) to approximately 53 miles (85 kilometers) above the Earth's surface. Therefore, the distance from the ground to the bottom of the mesosphere is roughly 31 miles. This layer of the atmosphere is characterized by a decrease in temperature with increasing altitude.
The mesosphere starts at an altitude of about 31 miles (50 kilometers) above the Earth's surface and extends up to about 53 miles (85 kilometers) high. This layer is characterized by decreasing temperatures with altitude.
The zone - or layer - that sits above the stratosphere is the mesosphere. This layer extends from about 50 km (or 31 miles) to around 85 km (or 53 miles) above the surface of the Earth. The mesosphere is where meteors will burn up as they enter the atmosphere. The temperature of this layer decreases with height.
between 30 and 50 miles
The stratosphere stops and the mesosphere starts at about 31 miles (50km). The mesosphere stops and the thermosphere starts at 50 - 56 miles (80 - 90 km).
The atmosphere above the stratosphere is called the mesosphere. It extends from about 50 kilometers (31 miles) to approximately 85 kilometers (53 miles) above the Earth's surface. In this layer, temperatures decrease with altitude, and it is where most meteors burn up upon entering the Earth's atmosphere. The mesosphere is followed by the thermosphere, which is characterized by a significant increase in temperature with height.
The temperature at the upper limit of the mesosphere, known as the mesopause, typically reaches around -90 degrees Celsius (-130 degrees Fahrenheit). This layer is situated approximately 85 to 100 kilometers (53 to 62 miles) above Earth's surface. The temperature decreases with altitude in the mesosphere, making it the coldest part of the Earth's atmosphere.
The mesosphere is the third layer of the Earth's atmosphere, located above the stratosphere and below the thermosphere. It extends from about 31 miles (50 kilometers) to 53 miles (85 kilometers) above the Earth's surface.
It is the Troposphere. The tropopause separates the troposphere (the lowest level of the atmosphere) from the stratosphere. It can be identified by the temperature of the air -- while in the troposphere, temperature decreases as you gain altitude; in the stratosphere, temperature increases as you gain altitude.
The layer of the atmosphere located above the stratosphere is the mesosphere. It extends from about 31 miles (50 kilometers) to 53 miles (85 kilometers) above the Earth's surface. The mesosphere is colder than the stratosphere and is where most meteors burn up upon entering the Earth's atmosphere.