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  2. Climate: Long range Investigation, Mapping, and Prediction

    en.wikipedia.org/wiki/Climate:_Long_range...

    CLIMAP map of ice sheets, sea temperature changes, and changes in the outline of coastal regions during the last glacial. Climate: Long range Investigation, Mapping, and Prediction , known as CLIMAP , was a major research project of the 1970s and 80s to produce a map of climate conditions during the Last Glacial Maximum .

  3. Kame delta - Wikipedia

    en.wikipedia.org/wiki/Kame_delta

    A kame delta (or ice-contact delta, morainic delta [1]) is a glacial landform formed by a stream of melt water flowing through or around a glacier and depositing material, known as kame (stratified sequence of sediments) deposits.

  4. Ice-sheet model - Wikipedia

    en.wikipedia.org/wiki/Ice-sheet_model

    The fourth IPCC assessment report showed ice-sheet models with projections of rapid dynamical responses in the ice, which led to evidence of significant ice loss. [ 2 ] In 2016, part of the Coupled Model Intercomparison Project Phase 6 (CMIP Phase 6) was the Ice Sheet Model Intercomparison Project , which defined a protocol for all variables ...

  5. Cordilleran ice sheet - Wikipedia

    en.wikipedia.org/wiki/Cordilleran_ice_sheet

    The rapid retreat of the Cordilleran ice sheet is a focus of study by glaciologists seeking to understand the difference in patterns of melting in marine-terminating glaciers, glaciers whose margin extends into open water without seafloor contact, and land-terminating glaciers, with a land or seafloor margin, as scientists believe the western ...

  6. 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.

  7. Glacier morphology - Wikipedia

    en.wikipedia.org/wiki/Glacier_morphology

    [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] They feature a higher velocity in the centre of the stream, and are bounded by slow-moving ice on either side. [ 10 ]