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).
Temperature decreases with altitude in the mesosphere due to the decrease in atmospheric pressure with height. This is because the mesosphere is above the stratosphere where the ozone layer absorbs incoming solar radiation, leading to a decrease in temperature as altitude increases.
The mesosphere is the third layer of the Earth's atmosphere, located above the stratosphere and below the thermosphere. Temperatures in the mesosphere can range from as low as about -90 degrees Celsius to as high as -10 degrees Celsius, depending on various factors such as altitude and time of day.
The temperature in the mesosphere decreases with altitude, reaching its lowest point at the mesopause, the boundary between the mesosphere and thermosphere. This cooling effect is due to the diminishing density of gas molecules in this region.
The temperatures in the mesosphere vary mostly by altitude (and of course by season and latitude). The temperature of the upper mesosphere may fall as low as −101 °C (172 K; −150 °F). The temperatures in the lower mesosphere tend to be around the freezing point of water: 0 °C (273 K, 32 °F)
The layer immediately above the stratosphere is the mesosphere. It lies between the stratosphere and the thermosphere in Earth's atmosphere. The mesosphere is characterized by decreasing temperatures with altitude.
80km-90km
Temperature decreases with altitude in the mesosphere due to the decrease in atmospheric pressure with height. This is because the mesosphere is above the stratosphere where the ozone layer absorbs incoming solar radiation, leading to a decrease in temperature as altitude increases.
The stratosphere's temperature increases as altitude increases. The mesosphere's temperature decreases as it's altitude increases. This is helpful
The mesosphere is the third layer of the Earth's atmosphere, located above the stratosphere and below the thermosphere. Temperatures in the mesosphere can range from as low as about -90 degrees Celsius to as high as -10 degrees Celsius, depending on various factors such as altitude and time of day.
The temperature in the mesosphere decreases with altitude, reaching its lowest point at the mesopause, the boundary between the mesosphere and thermosphere. This cooling effect is due to the diminishing density of gas molecules in this region.
The temperatures in the mesosphere vary mostly by altitude (and of course by season and latitude). The temperature of the upper mesosphere may fall as low as −101 °C (172 K; −150 °F). The temperatures in the lower mesosphere tend to be around the freezing point of water: 0 °C (273 K, 32 °F)
The temperature decreases
the altitude is 10 negative 85 km
The layer immediately above the stratosphere is the mesosphere. It lies between the stratosphere and the thermosphere in Earth's atmosphere. The mesosphere is characterized by decreasing temperatures with altitude.
In the troposphere, temperature typically decreases with increasing altitude due to the adiabatic cooling effect. In the mesosphere, temperature increases with altitude due to absorption of solar radiation by ozone molecules.
It is 87 km of altitude.
The Earth's atmosphere is divided into five primary layers: the troposphere, stratosphere, mesosphere, thermosphere, and exosphere. Each layer has distinct characteristics, such as temperature changes, composition, and altitude range.