Примери за използване на Ice shelf на Английски и техните преводи на Български
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The response of the ice shelf tells us that we can track extremely sensitive details about it.”.
Next articleAntarctic ice shelf destabilized as race for Ancient Alien artifacts& new weapons heats up.
Environmental scientists had been following the development of a large crack in the Larsen's ice shelf for over a decade.
The Larsen C Ice Shelf in Antarctica is cut through by a growing rift,
The warm water that is melting the ice shelf from underneath was pushed up from the deep ocean, Lhermitte said.
NASA informed us six months ago that the Western Antarctic Ice Shelf is now disintegrating.
If the ice shelf deteriorates as the Larsen B Ice Shelf did in 2002,
The response of the ice shelf tells us that we can track extremely sensitive details about it," Chaput said.
floating on the water and forming an ice shelf.
According to MIDAS researchers, when the iceberg separates, the Larsen C Ice Shelf will lose more than 10 percent of its area- about 2,000 square miles(5,000 square km).
If the giant iceberg-calving event about to occur destabilizes the ice shelf, it could result in the rapid flow of the land-based glaciers behind it into the ocean.
This satellite transmitter will help to track the continued break-up of this colossal ice shelf.
As the South Pole's fourth-largest ice shelf, the Larsen C Ice Shelf holds back many land-based glaciers just behind it, according to scientists.
Icebergs can be detach from the floating part of the glacier, or ice shelf, and can be as thick as the entire ice shelf is tall.
These are the same kinds of pools that formed here, on this ice shelf in Antarctica.
inevitably the ice shelf will crack and send a large iceberg free.
The seawater froze to the ice shelf, and because it contained dissolved organic matter,
But she said this just before we started heading right towards a giant wall of ice, like a ice shelf.
Calving at the end of an ice shelf can form plate icebergs with surface areas of up to hundreds of square kilometres.
the below-sea-level point where the ice shelf locks onto the continental bedrock.