Ví dụ về việc sử dụng Ice shelves trong Tiếng anh và bản dịch của chúng sang Tiếng việt
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Ice shelves are found in Antarctica, Greenland and Canada only.
The ice shelf, called Larsen C,is one of Antarctica's largest ice shelves.
Ice shelves are found only in Antarctica, Greenland, and Canada.
On the Antarctic Peninsula, a one-degree sea temperaturerise has helped to break apart seven major ice shelves in the last 30 years.
Ice shelves are extensions of glaciers and function as barriers.
The effects of melt ponds are diverse(this subsectionrefers to melt ponds on ice sheets and ice shelves).
The Larsen A and B ice shelves collapsed in 1995 and 2002 respectively.
This is especially important in regions next to thestrongly warming Antarctic Peninsula where some ice shelves have dramatically broken away into the ocean.
Other prominent ice shelves in the region also have been affected over the years.
On reaching the sea, these glaciers fracture and release icebergs orform large regions of floating ice known as ice shelves.
The Larsens A and B ice shelves collapsed, respectively, in 1995 and 2002.
Ice shelves surrounding the continent hold back ice like the Hoover Dam.
The Larsen A and B ice shelves, situated further north on the Antarctic Peninsula, collapsed in 1995 and 2002.
Seven ice shelves along the Antarctic Peninsula have retreated or disintegrated in the last two decades.
In recent years, several ice shelves have cracked up around northern parts of Antarctica, including the Larsen B that disintegrated in 2002.
These ice shelves stabilize the ice sheets- but when they break off, they can create an unstable situation.
Various ice shelves, including the Filchner-Ronne Ice Shelf, fringe the Weddell sea.
Larsen A and B ice shelves, which were situated further north on the Antarctic Peninsula, collapsed in 1995 and 2002.
Typically, ice shelves lose mass by iceberg calving and by melting at their upper and lower surfaces.
Ice shelves are found where glaciers meet the ocean and the climate is cold enough to sustain the ice as it goes afloat.
Ice shelves in the Arctic lost more than 90% of their total surface area during the 20th century and are continuing to disintegrate rapidly.
Ice shelves in the region have lost almost one fifth of their thickness in the last two decades, thereby reducing the resisting force on the glaciers.
Ice shelves in the region have lost roughly 1/5 of their thickness in the last twenty years which has attributed to reducing the resistance force of the glaciers.
If ice shelves are removed from the system, the ice sheet will rapidly accelerate towards the ocean, bringing about further ice mass loss.
Antarctic ice shelves have been thinning at an overall rate of about 300 cubic km per year between 2003 and 2012 and are projected to thin even further over the 21st century.
Predicting how quickly ice shelves break up and form icebergs is less well understood and is currently one of the biggest uncertainties in future Antarctic mass loss.
For example, ice shelves along the coast of the Amundsen and Bellingshausen Seas are the most rapidly thinning and have the smallest“safety bands” of all Antarctic ice shelves.
In the early 2000s, ice shelves began disintegrating in several parts of Antarctica, and scientists realized that process could greatly accelerate the demise of the vastly larger ice sheets themselves.