| 释义 |
Definition of ice front in English: ice frontnoun The lower edge of a glacier. Example sentencesExamples - During the middle of summer a camp was established just below the ice front, in preparation for the collection of watersamples.
- The dark band just north of the ice front is a narrow stretch of open water called a lead.
- By using a GIS platform to store and digitize the images, we were able to easily compare temporal changes among ice fronts.
- About 15,500 years ago, the ice front had cleared the Lake Erie basin, but advanced again to recover that area and more by 14,800 years ago.
- The total length of their ice fronts is 2510 km, 443 km, and 230 km, respectively.
- The ice front will remain in the same place as long as the rate of accumulation is equal to the rate of melting.
- Here one was pent in by steep mountain walls and the great ice fronts of the Jätte and De Geer Glaciers, which descend from the Inland Ice.
- As water undermines the ice fronts, great blocks of ice up to 200 feet high break loose and crash into the water.
- In total approximately 10,000 square kilometres of ice had broken off along the 300 km long ice front.
- This debris accumulated at the ice front building thick ridges of unconsolidated sediment.
- Labels of ice front positions denote cores collected in 1994-95.
- As water undermines some ice fronts, great blocks of ice up to 200 feet high break loose and crash into the water.
- A special front-tracking technique is used to compute the motion of the cell membrane and the ice front during freezing.
- The proposed research will produce the first direct numerical simulations of the interaction of non-planar ice fronts with deformable cells.
- It is known that Pleistocene animals retreated from advancing ice fronts, or glacier, and followed retreating ice fronts.
- High frequency ice divergence is dominated by ice response to wind stress rather than by tides except along the shelf break and ice fronts.
- A wave of intracellular ice nucleation in 100% of the cells followed the extracellular ice front across the field of view.
- These data represent the most complete, near-contemporaneous sampling of conditions at both ice fronts that has been made to date.
- For example, compressive stresses near ice fronts may cause folding or thrusting of basal debris to the ablating ice surface.
- This was followed by a readvance of glaciers down major fjords and subsequent retreat to present ice fronts.
Definition of ice front in US English: ice frontnoun The lower edge of a glacier. Example sentencesExamples - Here one was pent in by steep mountain walls and the great ice fronts of the Jätte and De Geer Glaciers, which descend from the Inland Ice.
- For example, compressive stresses near ice fronts may cause folding or thrusting of basal debris to the ablating ice surface.
- During the middle of summer a camp was established just below the ice front, in preparation for the collection of watersamples.
- As water undermines the ice fronts, great blocks of ice up to 200 feet high break loose and crash into the water.
- About 15,500 years ago, the ice front had cleared the Lake Erie basin, but advanced again to recover that area and more by 14,800 years ago.
- This was followed by a readvance of glaciers down major fjords and subsequent retreat to present ice fronts.
- It is known that Pleistocene animals retreated from advancing ice fronts, or glacier, and followed retreating ice fronts.
- A wave of intracellular ice nucleation in 100% of the cells followed the extracellular ice front across the field of view.
- The total length of their ice fronts is 2510 km, 443 km, and 230 km, respectively.
- The ice front will remain in the same place as long as the rate of accumulation is equal to the rate of melting.
- These data represent the most complete, near-contemporaneous sampling of conditions at both ice fronts that has been made to date.
- Labels of ice front positions denote cores collected in 1994-95.
- In total approximately 10,000 square kilometres of ice had broken off along the 300 km long ice front.
- The dark band just north of the ice front is a narrow stretch of open water called a lead.
- This debris accumulated at the ice front building thick ridges of unconsolidated sediment.
- As water undermines some ice fronts, great blocks of ice up to 200 feet high break loose and crash into the water.
- High frequency ice divergence is dominated by ice response to wind stress rather than by tides except along the shelf break and ice fronts.
- A special front-tracking technique is used to compute the motion of the cell membrane and the ice front during freezing.
- By using a GIS platform to store and digitize the images, we were able to easily compare temporal changes among ice fronts.
- The proposed research will produce the first direct numerical simulations of the interaction of non-planar ice fronts with deformable cells.
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