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  2. Polar ice cap - Wikipedia

    en.wikipedia.org/wiki/Polar_ice_cap

    The composition of the ice will vary. For example, Earth's polar caps are mainly water ice, whereas Mars's polar ice caps are a mixture of solid carbon dioxide and water ice. Polar ice caps form because high-latitude regions receive less energy in the form of solar radiation from the Sun than equatorial regions, resulting in lower surface ...

  3. Martian polar ice caps - Wikipedia

    en.wikipedia.org/wiki/Martian_polar_ice_caps

    1995 photo of Mars showing approximate size of the polar caps. The planet Mars has two permanent polar ice caps of water ice and some dry ice (frozen carbon dioxide, CO 2).Above kilometer-thick layers of water ice permafrost, slabs of dry ice are deposited during a pole's winter, [1] [2] lying in continuous darkness, causing 25–30% of the atmosphere being deposited annually at either of the ...

  4. Arctic ice pack - Wikipedia

    en.wikipedia.org/wiki/Arctic_ice_pack

    Currently, 28% of Arctic basin sea ice is multi-year ice, [2] thicker than seasonal ice: up to 3–4 m (9.8–13.1 ft) thick over large areas, with ridges up to 20 m (65.6 ft) thick. Besides the regular seasonal cycle there has been an underlying trend of declining sea ice in the Arctic in recent decades as well.

  5. Antarctic ice sheet - Wikipedia

    en.wikipedia.org/wiki/Antarctic_ice_sheet

    It is believed that the loss of the ice sheet would take between 2,000 and 13,000 years, although several centuries of high emissions may shorten this to 500 years. 3.3 m (10 ft 10 in) of sea level rise would occur if the ice sheet collapses but leaves ice caps on the mountains behind, and 4.3 m (14 ft 1 in) if those melt as well.

  6. Arctic geoengineering - Wikipedia

    en.wikipedia.org/wiki/Arctic_geoengineering

    It has been proposed to actively enhance the polar ice cap by spraying or pumping water onto the top of it which would build thicker sea ice. [13] [14] [15] A benefit of this method is that the increased salt content of the melting ice will tend to strengthen downwelling currents when the ice re-melts. [16] Some ice in the sea is frozen seawater.

  7. Past sea level - Wikipedia

    en.wikipedia.org/wiki/Past_sea_level

    This acceleration is 3 times larger than for mountain glaciers and ice caps (12 ± 6 Gt/yr²). [4] Ice shelves float on the surface of the sea and, if they melt, to first order they do not change sea level. Likewise, the melting of the northern polar ice cap which is composed of floating pack ice would not significantly contribute to rising sea ...

  8. Global warming likely to cause colder and snowier winters ...

    www.aol.com/news/2014-09-15-global-warming...

    The "polar vortex" that plunged Canada and the U.S. into historical cold last winter is said by researchers to have occurred because melting polar ice changes weather patterns, according to a ...

  9. Planum Boreum - Wikipedia

    en.wikipedia.org/wiki/Planum_Boreum

    Light browns are layers of surface dust greys and blues are layers of water and carbon dioxide ice. Regular geometric cracking is indicative of higher concentrations of water ice. The main feature of the Planum Boreum is a large fissure or canyon in the polar ice cap called Chasma Boreale. It is up to 100 kilometres (62 mi) wide and features ...