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  2. Glacial motion - Wikipedia

    en.wikipedia.org/wiki/Glacial_motion

    Seasonal melt ponding and penetrating under glaciers shows seasonal acceleration and deceleration of ice flows affecting whole icesheets. [ 3 ] Some glaciers experience glacial quakes —glaciers "as large as Manhattan and as tall as the Empire State Building , can move 10 meters in less than a minute, a jolt that is sufficient to generate ...

  3. Surface runoff - Wikipedia

    en.wikipedia.org/wiki/Surface_runoff

    Surface runoff is defined as precipitation (rain, snow, sleet, or hail [5]) that reaches a surface stream without ever passing below the soil surface. [6] It is distinct from direct runoff, which is runoff that reaches surface streams immediately after rainfall or melting snowfall and excludes runoff generated by the melting of snowpack or ...

  4. Eustatic sea level - Wikipedia

    en.wikipedia.org/wiki/Eustatic_sea_level

    Changes in total ocean water mass, for instance, by ice-sheet runoff. When an ice sheet (such as Greenland) begins to lose some of its ice mass due to melt, the liquid water is transported to the ocean. [5] According to the "bathtub approach", ice-sheet runoff from Greenland will affect eustatic sea level in all areas of the world, whether ...

  5. Glacier - Wikipedia

    en.wikipedia.org/wiki/Glacier

    Glacial speed is affected by factors such as slope, ice thickness, snowfall, longitudinal confinement, basal temperature, meltwater production, and bed hardness. A few glaciers have periods of very rapid advancement called surges. These glaciers exhibit normal movement until suddenly they accelerate, then return to their previous movement state ...

  6. Glacier mass balance - Wikipedia

    en.wikipedia.org/wiki/Glacier_mass_balance

    Application of the model to Bering Glacier in Alaska demonstrated a close agreement with ice volume loss for the 1972–2003 period measured with the geodetic method. Determining the mass balance and runoff of the partially debris-covered Langtang Glacier in Nepal demonstrates an application of this model to a glacier in the Himalayan Range. [37]

  7. Basal sliding - Wikipedia

    en.wikipedia.org/wiki/Basal_sliding

    Basal sliding is the act of a glacier sliding over the bed due to meltwater under the ice acting as a lubricant.This movement very much depends on the temperature of the area, the slope of the glacier, the bed roughness, the amount of meltwater from the glacier, and the glacier's size.

  8. Snowmelt - Wikipedia

    en.wikipedia.org/wiki/Snowmelt

    Predicting snowmelt runoff from a drainage basin may be a part of designing water control projects. Rapid snowmelt can cause flooding. If the snowmelt is then frozen, very dangerous conditions and accidents can occur, introducing the need for salt to melt the ice.

  9. Evapotranspiration - Wikipedia

    en.wikipedia.org/wiki/Evapotranspiration

    Evapotranspiration (ET) refers to the combined processes which move water from the Earth's surface (open water and ice surfaces, bare soil and vegetation) into the atmosphere. [ 2 ] : 2908 It covers both water evaporation (movement of water to the air directly from soil, canopies , and water bodies) and transpiration (evaporation that occurs ...