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  2. Atmosphere - Wikipedia

    en.wikipedia.org/wiki/Atmosphere

    An atmosphere (from Ancient Greek ἀτμός (atmós) 'vapour, steam' and σφαῖρα (sphaîra) 'sphere') [1] is a layer of gases that envelop an astronomical object, held in place by the gravity of the object. A planet retains an atmosphere when the gravity is great and the temperature of the atmosphere is low.

  3. Atmosphere of Earth - Wikipedia

    en.wikipedia.org/wiki/Atmosphere_of_Earth

    The exosphere is the outermost layer of Earth's atmosphere (though it is so tenuous that some scientists consider it to be part of interplanetary space rather than part of the atmosphere). It extends from the thermopause (also known as the "exobase") at the top of the thermosphere to a poorly defined boundary with the solar wind and ...

  4. Atmospheric science - Wikipedia

    en.wikipedia.org/wiki/Atmospheric_science

    The composition of the Earth's atmosphere is different from the other planets because the various life processes that have transpired on the planet have introduced free molecular oxygen. [7] Much of Mercury's atmosphere has been blasted away by the solar wind. [8] The only moon that has retained a dense atmosphere is Titan.

  5. Category:Atmosphere of Earth - Wikipedia

    en.wikipedia.org/wiki/Category:Atmosphere_of_Earth

    العربية; Arpetan; تۆرکجه; বাংলা; 閩南語 / Bân-lâm-gú; Башҡортса; Беларуская; Беларуская (тарашкевіца)

  6. Indonesia - Wikipedia

    en.wikipedia.org/wiki/Indonesia

    Indonesia, [b] officially the Republic of Indonesia, [c] is a country in Southeast Asia and Oceania, between the Indian and Pacific oceans. It consists of over 17,000 islands , including Sumatra , Java , Sulawesi , and parts of Borneo and New Guinea .

  7. Meteorology - Wikipedia

    en.wikipedia.org/wiki/Meteorology

    Dynamic meteorology generally focuses on the fluid dynamics of the atmosphere. The idea of air parcel is used to define the smallest element of the atmosphere, while ignoring the discrete molecular and chemical nature of the atmosphere. An air parcel is defined as an infinitesimal region in the fluid continuum of the atmosphere. The fundamental ...

  8. Mesosphere - Wikipedia

    en.wikipedia.org/wiki/Mesosphere

    Within the mesosphere, temperature decreases with increasing height.This is a result of decreasing absorption of solar radiation by the rarefied atmosphere having a diminishing relative ozone concentration as altitude increases (ozone being the main absorber in the UV wavelengths that survived absorption by the thermosphere). [7]

  9. Category:Atmosphere - Wikipedia

    en.wikipedia.org/wiki/Category:Atmosphere

    Anarâškielâ; العربية; Aragonés; Arpetan; Azərbaycanca; تۆرکجه; বাংলা; 閩南語 / Bân-lâm-gú; Basa Banyumasan; Башҡортса