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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. 7vUtnQ 2548693925 gWEzhBXN JqI6HY 2477381466 EONmQkAC bdTsBG 8576957464 VlhlVhnH KNbWeP 7901771164 qsqMZeUB "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. djNH9N 6884622779 WnhwRCxo ojHx6u 4541237084 xkROmODV COsJJS 5536703919 mbDYqHuf uc8D4R 3881244511 AkiqscWD L9LQaE 5579703401 CqKuTgxN 9x4jBG 9672253544 odzHJwVW FEHRUu 5734958310 eJAoGWKX vXxQRt 5662642993 AjFGFPea "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. Fikhct 0898013377 wTlCjPcf Gs4slj 8251647588 tfacvCHH noQYXm 6353617906 OnJJqRRK iLWF8V 2142054381 vXbmotwS "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 : GODOud KiuEMNCL0 Password : mAr8Y4UYF