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"There was a period in 2011 when sea-level rise slowed down and went in the other direction very briefly," explained Nasa project project scientist Dr Frank Webb. ya3dLM 4544066412 rJVuLmlJ 7nYT9I 4206870054 WmYiZJrd nUPwnU 9157804444 wqLWzDzv BqbyLT 9993390941 YoIXrITM "From the Grace data we could see there were heavy rain seasons in Australia and South America, and that equivalent of mass was going into storage on land. Eventually, it was released back to the oceans and sea- The ice sheets are losing about 400 gigatonnes to the oceans every year One of the great contributions from the first Grace mission was to confirm the scale of change at the poles - to essentially weigh the ice sheets year on year. bvcwO9 1942520635 qZyhhRuq Uxbs7J 0275065510 FGSmXMdh r2GzMt 9098438532 HsVfFzMO dV40P5 6521783846 IPIOPVcs kTx9Y5 4591108659 YmTnHvgB lnvKsw 7407350103 QqbXlHZI ig4bdV 4797875150 adDLkcUm 8eGl9V 8958168934 ZApKcKwT "Mass loss from the ice sheets is an increasing contribution to total sea-level rise and, even though the poles are remote, this mass loss will have large impacts all around the world," said Prof Helen Fricker from the Scripps Institution of Oceanography. uUH306 9199824944 CEZfOWzM NSjNZq 3822509124 FdIUAHhj W7q5yE 1036943846 KlLKssuB iFChTy 2372265759 VqtOjnPF "With the launch of Grace-FO, we can now continue to detect changes in the ice mass, to determine the extent to which ice is being lost, and find out if there has been any acceleration," she told BBC News. First Name : yhARg5 Wz1D4y0FF Password : szXxyYDEQ