{"id":34224,"date":"2020-01-29T03:00:05","date_gmt":"2020-01-29T02:00:05","guid":{"rendered":"https:\/\/www.cde.ual.es\/?p=34224"},"modified":"2020-01-28T11:30:05","modified_gmt":"2020-01-28T10:30:05","slug":"cryosat-brings-us-closer-to-understanding-what-happens-in-the-antarcticas-biggest-glacier","status":"publish","type":"post","link":"https:\/\/www.cde.ual.es\/en\/cryosat-brings-us-closer-to-understanding-what-happens-in-the-antarcticas-biggest-glacier\/","title":{"rendered":"CryoSat brings us closer to understanding what happens in the Antarctica\u2019s biggest glacier"},"content":{"rendered":"

Ice loss from Pine Island Glacier<\/strong> has contributed more to sea-level rise<\/strong> over the past four decades than any other glacier in Antarctica.<\/p>\n

\"\"<\/a><\/p>\n

The way this huge glacier is thinning is complex, leading to uncertainty about how it is likely to raise sea level in the future. Thanks to ESA\u2019s CryoSat mission, scientists have now been able to shed new light on these complex patterns of ice loss.<\/p>\n

Challenge<\/h3>\n

Although Pine Island Glacier is one of the most intensively and extensively investigated glacier systems in Antarctica, different model projections of future mass loss give conflicting results. Some suggest mass loss could dramatically increase over the next few decades, resulting in a rapidly growing contribution to sea level, while others indicate a more moderate response.<\/p>\n

Identifying which is the more likely behaviour is important for understanding future sea-level rise and how this vulnerable part of Antarctica is going to evolve over the coming decades.<\/p>\n

Results<\/h3>\n

In a paper published in Nature Geoscience, scientists from the University of Bristol, UK, describe how they used information from CryoSat to help clarify the situation. They discovered that the pattern of ice loss is evolving in complex ways, both in space and time.
\nRates in the fast-flowing central trunk of the glacier have decreased by about a factor of five since 2007 \u2013 and this is the opposite of what was observed prior to 2010.<\/p>\n

These new results suggest that rapid migration of the grounding line, the place where the grounded ice first meets the ocean, is unlikely over the next decades, without a major change in the role of the ocean in ice loss. Instead, the results support model simulations that imply that the glacier will continue to lose mass, but not at much greater rates than present.<\/p>\n

Lead author Prof. Jonathan Bamber from the University of Bristol\u2019s School of Geographical Sciences, said, \u201cThis could seem like a \u2018good news story\u2019, but it\u2019s important to remember that we still expect this glacier to continue to lose mass in the future and for that trend to increase over time, just not quite as fast as some model simulations suggested.\u201d<\/em><\/p>\n

Tommaso Parrinello, ESA\u2019s CryoSat mission manger, added, \u201cIn April, CryoSat will have been in orbit for 10 years, far exceeding its expected life. We continue to be proud of the contribution to science this extraordinary satellite mission is making.\u201d<\/em>\u00a0and \u201cCryoSat has helped clarify the situation at Pine Island Glacier, which is not only important for our scientific understanding, but ultimately for society at large.\u201d<\/em><\/p>\n

More information<\/h3>\n

Full news<\/a><\/p>\n

Paper<\/a><\/p>\n","protected":false},"excerpt":{"rendered":"

Ice loss from Pine Island Glacier has contributed more to sea-level rise over the past four decades than any other glacier in Antarctica. The way this huge glacier is thinning is complex, leading to uncertainty about how it is likely to raise sea level in the future. 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