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The Atmosphere

Teacher: Dara de Castro
Horizontales
a layer of gases surrounding a planet or other material body of sufficient mass[3] that is held in place by the gravity of the body
balance sheet of energy income against expenditure
just above the troposphere, and below the mesosphere
the lowest portion of Earth's atmosphere
a region of Earth's stratosphere that absorbs most of the Sun's UV radiation
the concerted, collective movement of groups or aggregates of molecules within fluids (e.g., liquids, gases) and rheids, either through advection or through diffusion or as a combination of both of them
Verticales
the layer of the Earth's atmosphere directly above the mesosphere and directly below the exosphere.
the layer of the Earth's atmosphere that is directly above the stratopause and directly below the mesopause
the transfer of internal energy by microscopic diffusion and collisions of particles or quasi-particles within a body due to a temperature gradient
a process in which electromagnetic waves (EMR) travel through a vacuum or through matter-containing media