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  2. Ice sheet - Wikipedia

    en.wikipedia.org/wiki/Ice_sheet

    Greenland ice sheet as seen from space. An ice sheet is a body of ice which covers a land area of continental size - meaning that it exceeds 50,000 km 2. [4] The currently existing two ice sheets in Greenland and Antarctica have a much greater area than this minimum definition, measuring at 1.7 million km 2 and 14 million km 2, respectively.

  3. Cryosphere - Wikipedia

    en.wikipedia.org/wiki/Cryosphere

    The mass balance of land-based glaciers and ice sheets is determined by the accumulation of snow, mostly in winter, and warm-season ablation due primarily to net radiation and turbulent heat fluxes to melting ice and snow from warm-air advection [13] [14] Where ice masses terminate in the ocean, iceberg calving is the major contributor to mass ...

  4. Climate system - Wikipedia

    en.wikipedia.org/wiki/Climate_system

    The five components of the climate system all interact. They are the atmosphere, the hydrosphere, the cryosphere, the lithosphere and the biosphere. [1]: 1451 Earth's climate system is a complex system with five interacting components: the atmosphere (air), the hydrosphere (water), the cryosphere (ice and permafrost), the lithosphere (earth's upper rocky layer) and the biosphere (living things).

  5. Tipping points in the climate system - Wikipedia

    en.wikipedia.org/wiki/Tipping_points_in_the...

    Around half of the ice loss occurs via surface melting, and the remainder occurs at the base of the ice sheet where it touches the sea, by calving (breaking off) icebergs from its margins. [28] The Greenland ice sheet has a tipping point because of the melt-elevation feedback. Surface melting reduces the height of the ice sheet, and air at a ...

  6. Antarctic ice sheet - Wikipedia

    en.wikipedia.org/wiki/Antarctic_ice_sheet

    It is the largest of Earth's two current ice sheets, containing 26.5 million cubic kilometres (6,400,000 cubic miles) of ice, which is equivalent to 61% of all fresh water on Earth. Its surface is nearly continuous, and the only ice-free areas on the continent are the dry valleys, nunataks of the Antarctic mountain ranges , and sparse coastal ...

  7. Ice-sheet model - Wikipedia

    en.wikipedia.org/wiki/Ice-sheet_model

    Ice sheets interact with the surrounding atmosphere, ocean and sub-glacial earth. [15] All of these interactive components need to be included to be able to have a comprehensive ice-sheet model. [15] Basal Conditions play an important role in determining the behavior of ice sheets.

  8. Effects of climate change on the tropics - Wikipedia

    en.wikipedia.org/wiki/Effects_of_climate_change...

    NASA plays a critical role in providing the scientific data necessary for understanding and addressing climate change globally. Through missions like GRACE, ICESat, and Sentinel-6, NASA documents crucial changes in the Earth's ice sheets and sea levels, offering invaluable insights for both mitigation and adaptation efforts. Although not ...

  9. Atmosphere of Earth - Wikipedia

    en.wikipedia.org/wiki/Atmosphere_of_Earth

    The atmosphere of Earth is composed of a layer of gas mixture that surrounds the Earth's planetary surface (both lands and oceans), known collectively as air, with variable quantities of suspended aerosols and particulates (which create weather features such as clouds and hazes), all retained by Earth's gravity.