This article is about the atmospheric mesosphere, for the Earth' mantle see
Mesosphere (mantle). The mesosphere (from the
Greek words mesos = middle and sphaira = ball) is the layer of the
Earth's atmosphere that is directly above the
stratosphere and directly below the
thermosphere. The mesosphere is located from about 50 km to 80-90 km altitude above
Earth's surface. Within this layer, temperature decreases with increasing
altitude. The main dynamical features in this region are
atmospheric tides, internal atmospheric gravity waves (usually just called "
gravity waves") and
planetary waves. Most of these waves and tides are excited in the
troposphere and lower
stratosphere and propagate upward to the mesosphere. In the mesosphere, gravity-wave amplitudes can become so large that the waves' dissipation transmits so much energy that it largely drives the global circulation of the mesosphere.
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