However, the British researchers used satellite images and radar data to measure the disparity in the height of the Filchner- Ronne Ice Shelf in West Antartica.
The torrent of water forms the beneath ice on solid land, said researchers. They are said that the cold meltwater linked at the ice shelf it will causes warmer sea water to trail upwards. It also describes that melt water arrives on land would flow into the sea in a thin layer which gets different effect on ice flow.
According to the Researchers said that the arrangement of water
