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  2. Atmosphere of Earth - Wikipedia

    en.wikipedia.org/wiki/Atmosphere_of_Earth

    The troposphere is the lowest layer of Earth's atmosphere. It extends from Earth's surface to an average height of about 12 km (7.5 mi; 39,000 ft), although this altitude varies from about 9 km (5.6 mi; 30,000 ft) at the geographic poles to 17 km (11 mi; 56,000 ft) at the Equator , [ 23 ] with some variation due to weather.

  3. File:Atmosphere layers-en.svg - Wikipedia

    en.wikipedia.org/wiki/File:Atmosphere_layers-en.svg

    Diagram of the five primary layers of the Earth's atmosphere (not to scale). From Earth's surface to top of stratosphere (50 km) is slightly less than1% of Earth's radius. Between troposphere & stratosphere is the tropopause.

  4. Atmosphere - Wikipedia

    en.wikipedia.org/wiki/Atmosphere

    Earth's atmosphere profile. The atmosphere of Earth is composed of layers with different properties, such as specific gaseous composition, temperature, and pressure. The troposphere is the lowest layer of the atmosphere. This extends from the planetary surface to the bottom of the stratosphere.

  5. File:Earth's atmosphere.svg - Wikipedia

    en.wikipedia.org/wiki/File:Earth's_atmosphere.svg

    The layers of the atmosphere are drawn to precise scale. Objects within them, such as the weather balloon are not. It is designed to be displaced at its native resolution (430×700px) or higher. It will render incorrectly (things start disappearing) below that.

  6. Mesosphere - Wikipedia

    en.wikipedia.org/wiki/Mesosphere

    From Earths surface to the top of the stratosphere (50 km) is just under 1% of Earth's radius. The mesosphere (/ ˈ m ɛ s ə s f ɪər, ˈ m ɛ z-, ˈ m iː s ə-,-z ə-/; [1] from Ancient Greek μέσος (mésos) 'middle' and -sphere) is the third layer of the atmosphere, directly above the stratosphere and directly below the thermosphere.

  7. Thermosphere - Wikipedia

    en.wikipedia.org/wiki/Thermosphere

    The density of the Earth's atmosphere decreases nearly exponentially with altitude. The total mass of the atmosphere is M = ρ A H ≃ 1 kg/cm 2 within a column of one square centimeter above the ground (with ρ A = 1.29 kg/m 3 the atmospheric density on the ground at z = 0 m altitude, and H ≃ 8 km the average atmospheric scale height).

  8. File:Atmospheric Layers.svg - Wikipedia

    en.wikipedia.org/wiki/File:Atmospheric_Layers.svg

    This file is licensed under the Creative Commons Attribution-Share Alike 3.0 Unported license.: You are free: to share – to copy, distribute and transmit the work; to remix – to adapt the work

  9. File:Atmosphere layers-nb.svg - Wikipedia

    en.wikipedia.org/wiki/File:Atmosphere_layers-nb.svg

    Image:Atmosphere layers.svg: Author: NOAA & Mysid (translated by Jon Harald Søby) Permission (Reusing this file) Public domain: Other versions (Multiple languages)