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  2. Glacier morphology - Wikipedia

    en.wikipedia.org/wiki/Glacier_morphology

    Ice streams rapidly channel ice flow out to the sea, ocean, or an ice shelf. For this reason, they are commonly referred to as the "arteries" of an ice sheet. [8] [9] Ice from continental sheets is drained into the ocean by a complex network of ice streams, and their activity is greatly affected by oceanic and atmospheric processes. [8]

  3. Sea ice - Wikipedia

    en.wikipedia.org/wiki/Sea_ice

    First-year sea ice is ice that is thicker than young ice but has no more than one year growth. In other words, it is ice that grows in the fall and winter (after it has gone through the new ice – nilas – young ice stages and grows further) but does not survive the spring and summer months (it melts away). The thickness of this ice typically ...

  4. Tipping points in the climate system - Wikipedia

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

    The Greenland ice sheet is the second largest ice sheet in the world, and the water which it holds, if completely melted, would raise sea levels globally by 7.2 metres (24 ft). [ 25 ] [ 26 ] Due to global warming, the ice sheet is melting at an accelerating rate, adding almost 1 mm to global sea levels every year. [ 27 ]

  5. Cryosphere - Wikipedia

    en.wikipedia.org/wiki/Cryosphere

    Overview of the cryosphere and its larger components [1]. The cryosphere is an umbrella term for those portions of Earth's surface where water is in solid form. This includes sea ice, ice on lakes or rivers, snow, glaciers, ice caps, ice sheets, and frozen ground (which includes permafrost).

  6. Glaciology - Wikipedia

    en.wikipedia.org/wiki/Glaciology

    ' study of ice ') is the scientific study of glaciers, or, more generally, ice and natural phenomena that involve ice. Glaciology is an interdisciplinary Earth science that integrates geophysics , geology , physical geography , geomorphology , climatology , meteorology , hydrology , biology , and ecology .

  7. Ice–albedo feedback - Wikipedia

    en.wikipedia.org/wiki/Ice–albedo_feedback

    Ice–albedo feedback is a climate change feedback, where a change in the area of ice caps, glaciers, and sea ice alters the albedo and surface temperature of a planet. Because ice is very reflective, it reflects far more solar energy back to space than open water or any other land cover . [ 1 ]

  8. Iceberg - Wikipedia

    en.wikipedia.org/wiki/Iceberg

    An iceberg in the Arctic Ocean Tabular iceberg Iceberg from overhead showing above and submerged ice. An iceberg is a piece of fresh water ice more than 15 meters (16 yards) long [1] that has broken off a glacier or an ice shelf and is floating freely in open water. [2] [3] Smaller chunks of floating glacially derived ice are called "growlers ...

  9. Effects of climate change on oceans - Wikipedia

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

    Global warming, caused by greenhouse gas forcing is responsible for the decline in Arctic sea ice. The decline of sea ice in the Arctic has been accelerating during the early twenty-first century, with a decline rate of 4.7% per decade (it has declined over 50% since the first satellite records). [74] [75] [76] Summertime sea ice will likely ...