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  2. Greenland ice sheet - Wikipedia

    en.wikipedia.org/wiki/Greenland_ice_sheet

    Another record was set in July 2012, when the melt zone extended to 97% of the ice sheet's cover, [123] and the ice sheet lost approximately 0.1% of its total mass (2900 Gt) during that year's melting season, with the net loss (464 Gt) setting another record. [124]

  3. Tipping points in the climate system - Wikipedia

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

    Examples of tipping points include thawing permafrost, which will release methane, a powerful greenhouse gas, or melting ice sheets and glaciers reducing Earth's albedo, which would warm the planet faster. Thawing permafrost is a threat multiplier because it holds roughly twice as much carbon as the amount currently circulating in the atmosphere.

  4. Post-glacial rebound - Wikipedia

    en.wikipedia.org/wiki/Post-glacial_rebound

    As well as the addition of melted ice water from glaciers and ice sheets, recent sea level changes are affected by the thermal expansion of sea water due to global warming, [28] sea level change due to deglaciation of the last glacial maximum (postglacial sea level change), deformation of the land and ocean floor and other factors. Thus, to ...

  5. Huge glacier melt and fast rising seas amid hottest eight ...

    www.aol.com/huge-glacier-melt-fast-rising...

    Glacier melt records were shattered in the European Alps, with average loss of three to four metres of ice thickness throughout the mountain range – substantially more than the previous record ...

  6. Melting of Alaska's Juneau icefield accelerates, losing snow ...

    www.aol.com/news/melting-alaskas-juneau-icefield...

    The melting of Alaska's Juneau icefield, home to more than 1,000 glaciers, is accelerating. The snow covered area is now shrinking 4.6 times faster than it was in the 1980s, according to a new study.

  7. Glacier mass balance - Wikipedia

    en.wikipedia.org/wiki/Glacier_mass_balance

    Ablation is the reverse of accumulation: it includes all the processes by which a glacier can lose mass. The main ablation process for most glaciers that are entirely land-based is melting; the heat that causes melting can come from sunlight, or ambient air, or from rain falling on the glacier, or from geothermal heat below the glacier bed.

  8. 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.

  9. Scientists just spotted unnerving melting beneath the ... - AOL

    www.aol.com/news/scientists-just-spotted...

    The Antarctic glacier has destabilized, retreating back nearly nine miles since the 1990s. If much of it progr Scientists just spotted unnerving melting beneath the 'Doomsday Glacier'