Mesosphere
Mesosphere
Based on the vertical temperature distribution in Earth's atmosphere, four semi-horizontal layers or "spheres" can be distinguished: the troposphere, stratosphere , mesosphere, and thermosphere,. These layers are separated by "pauses," where no change in the temperature occurs with altitude change: the tropopause (between the troposphere and the stratosphere), the stratopause (between the stratosphere and the mesosphere), and the mesopause (between the mesosphere and the thermosphere ). The stratosphere and mesosphere together are called the middle atmosphere, and their region also overlaps with the ionosphere , which is a region defined on the basis of the electric charges of the particles there.
The mesosphere, which means middle sphere, is the third layer of Earth's atmosphere, between the stratosphere, and the thermosphere. It is located from about 55 kilometers (35 miles) to 85 kilometers (54 miles) above the surface of Earth. Temperature here decreases with height, so within the mesosphere it is warmest at its lowest level (−5°C, or 23°F), and becomes coldest at its highest level (−80°C, or −112°F). Depending on latitude and season, temperatures in the upper mesosphere can be as low as −140°C (−220°F). The temperature in the mesosphere is lower than the temperature of the troposphere or stratosphere, which makes the mesosphere the coldest among the atmospheric layers. It is colder then Antarctica's lowest recorded temperature, and it is cold enough to freeze water vapor into ice clouds , which can be seen mostly after sunset.
Although the air in the mesosphere is relatively mixed, it is very thin, resulting in low atmospheric pressure . At this height, not only concentrations of ozone and water vapor are negligible, air in the mesosphere contains much less oxygen than in the troposphere. The mesosphere is also the layer in which many meteors burn up when they enter the earth's atmosphere, as a result of the collision with some of the gas particles present in this layer.
See also Atmospheric composition and structure; Stratosphere and stratopause; Thermosphere
mesosphere
1. Upper-atmospheric layer above the stratopause (at 50 km) through which temperature decreases with height up to about 80 km, where temperatures reach a minimum of about −90°C. This level is the mesopause, an inversion above which temperatures rise again. See also ATMOSPHERIC STRUCTURE.
2. That part of the Earth underlying the asthenosphere. The term is no longer in current use in this sense.
mesosphere
1. An upper atmospheric layer above the stratopause (at 50 km) through which temperature decreases with height up to about 80 km, where temperatures reach a minimum of about −90°. This level is the mesopause, an inversion above which temperatures rise again.
2. That part of the Earth underlying the asthenosphere. The term is no longer in current use in this sense.