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  2. Ice shelf - Wikipedia

    en.wikipedia.org/wiki/Ice_shelf

    The floating ice shelf is in the left foreground, and the grounding line is visible as an abrupt change in surface slope due to flexure caused by the buoyancy force where the ice reaches flotation. An ice shelf is a large platform of glacial ice floating on the ocean, fed by one or multiple tributary glaciers.

  3. Ice sheet - Wikipedia

    en.wikipedia.org/wiki/Ice_sheet

    As the ice shelf becomes thinner, it exerts less of a buttressing effect on the ice sheet, the so-called back stress increases and the grounding line is pushed backwards. [18] The ice sheet is likely to start losing more ice from the new location of the grounding line and so become lighter and less capable of displacing seawater.

  4. Radioglaciology - Wikipedia

    en.wikipedia.org/wiki/Radioglaciology

    Radioglaciology is the study of glaciers, ice sheets, ice caps and icy moons using ice penetrating radar.It employs a geophysical method similar to ground-penetrating radar and typically operates at frequencies in the MF, HF, VHF and UHF portions of the radio spectrum.

  5. Thwaites Glacier - Wikipedia

    en.wikipedia.org/wiki/Thwaites_Glacier

    Other labels refer to the ice tongue's grounding line, and northern and southern shear zones where it's in direct contact with the ice shelf. [ 29 ] The Thwaites Glacier Tongue, or Western Glacier Tongue ( 75°0′S 106°50′W  /  75.000°S 106.833°W  / -75.000; -106.833 ) was a narrow, floating part of the glacier, located about 30 ...

  6. Ross Ice Shelf - Wikipedia

    en.wikipedia.org/wiki/Ross_Ice_Shelf

    This re-freezing and growth of an ice shelf is not uncommon but the Ross Ice Shelf situation appeared to be very variable as there was no evidence of long-term freezing. [20] A recent study attribute this variability in-part to tidal mixing. [21] A second New Zealand expedition in 2019 traveled to the grounding line region of the Kamb Ice Stream.

  7. West Antarctic Ice Sheet - Wikipedia

    en.wikipedia.org/wiki/West_Antarctic_Ice_Sheet

    The grounding lines of its glaciers are below the sea level by several hundred metres or more, and the bed only deepens upstream. [33] This means that as the ice sheet loses mass to melting, an increasing fraction of its height becomes exposed to warm water flows that are no longer displaced by its mass.

  8. No $750 reward for using ICE tip line to report 'illegal ...

    www.aol.com/no-750-reward-using-ice-211747325.html

    The claim: ICE is offering $750 reward for reporting 'illegal immigrants' through tip line. A Jan. 20 Instagram post (direct link, archive link) claims U.S. Immigration and Customs Enforcement, or ...

  9. Pine Island Glacier - Wikipedia

    en.wikipedia.org/wiki/Pine_Island_Glacier

    In the 1940s, when the glacier started its retreat, [23] the grounding line of the glacier was on an undersea ridge approximately 47 kilometres (29 mi) downstream of its grounding line in 2023. [3] Of this retreat, 31 kilometres (19 mi) occurred between 1992 and 2011. [24] Pine Island Glacier calving Iceberg B-46 (226 km 2 or 87 sq mi).