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    Atmosphere of Earth - Wikipedia

    In this way, Earth's atmosphere can be divided (called atmospheric stratification) into five main layers: troposphere, stratosphere, mesosphere, thermosphere, and exosphere. The altitudes of the five layers are: Exosphere: 700 to 10,000 km (440 to 6,200 miles) Thermosphere: 80 to 700 km (50 to 440 miles) See more

    The atmosphere of Earth is the layer of gases, known collectively as air, retained by Earth's gravity that surrounds the planet and forms its … See more

    Composition image
    Optical properties image
    Circulation image

    In general, air pressure and density decrease with altitude in the atmosphere. However, the temperature has a more complicated profile … See more

    Solar radiation (or sunlight) is the energy Earth receives from the Sun. Earth also emits radiation back into space, but at longer wavelengths that humans cannot see. Part of the … See more

    Earliest atmosphere
    The first atmosphere consisted of gases in the solar nebula, primarily hydrogen. There were probably simple See more

    Evolution of Earth's atmosphere image
    Overview image

    The three major constituents of Earth's atmosphere are nitrogen, oxygen, and argon. Water vapor accounts for roughly 0.25% of the … See more

    Stratification image
    Physical properties image

    Pressure and thickness
    The average atmospheric pressure at sea level is defined by the International Standard Atmosphere as 101325 pascals (760.00 See more

    Atmospheric circulation is the large-scale movement of air through the troposphere, and the means (with ocean circulation) by which heat is distributed around Earth. The large-scale structure of the atmospheric circulation varies from year to year, but the basic … See more

     
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