Examples of using Ice sheets in English and their translations into Swedish
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Many scientists believe that the catastrophic episodes above were caused by rapid collapses of major ice sheets.
for sea level and ice sheets since about the past decade.
Sea level rise 55.0 m: if all ice sheets outside East Antarctic melt, plus 80% of East Antarctic.
will make the ice sheets of the Earth to expand with a special frequency?
This makes it possible to make detailed studies of the sea bottom at great depths and under 500-metre-thick ice sheets, environments previously inaccessible to researchers.
and it causes the ice sheets and glaciers around the world to melt even faster.
With the help of these models, they can ascertain how climate changes affect the ice sheets, both in the past and the future.
These communities are significant in that they often change the color of glaciers and ice sheets, impacting the reflectivity of the ice itself.
Widespread decreases in glaciers and ice caps have contributed to sea level rise(ice caps do not include contributions from the Greenland and Antarctic Ice Sheets).
which drain ice from the interior of the ice sheets.
This group of garments was inspired by shimmering ridges with soft, rounded stones formed under ice sheets.
The whole of Scotland was covered by ice sheets during the Pleistocene ice ages
North America was covered by ice sheets up to 3 km thick.
If the poles were to shift does the mile thick ice sheets move with them?
It's with a sense of urgency that the glacial scientific community is trying to understand the stability of marine ice sheets, and the ways in which marine ice sheet sectors may de-(or re-)stabilise in the future.
also on how glaciers and ice sheets work and their role in Earth's systems.
increased loss of mass from glaciers and ice sheets.
The melting of the ice sheets between 17,000 BCE and 5,000 BCE was no smooth process, but periods of rather slow sea level rise were interrupted by catastrophic episodes, where sea level could rise many meters in just a few centuries.
Meltwater pulses The melting of the ice sheets between 17,000 BCE and 5,000 BCE was no smooth process, but periods of rather slow sea level rise were interrupted by catastrophic episodes, where sea level could rise many meters in just a few centuries.
Map videos showing coastal areas around the world while all ice sheets melt, from the last glacial maximum,