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Co-lead Seabed Curtain Project, @UArctic Frozen Arctic Conservation Network |

Earth’s two large ice sheets, in Antarctica and Greenland, are currently deteriorating and will continue to deteriorate even under the most optimistic greenhouse-gas emissions scenarios. They are a major contributor to sea-level rise and the subsequent damage to natural and human systems. We cannot stop sea-level rise, but we may be able to slow it while humanity does the necessary shift away from carbon based energy systems. Over the last four decades, scientific research on ice-sheet deterioration and sea-level rise has been focused on two essential questions: 1. What physical processes cause ice-mass loss that contributes either directly or indirectly to sea-level rise? 2. How is climate change affecting these processes? Significant progress has been made on these scientifically (and logistically) challenging questions. Most notably, research has identified the physical instability processes that can accelerate ice-sheet mass loss leading to sea-level rise, even under steady or improving climate, as well as “hot spots” where instability may be happening now, e.g., the Thwaites Glacier in the Amundsen Sea sector of Antarctica. Answers to the above questions have recently raised three further questions that are argued to be essential in driving research over the next two decades. These questions are: 3. What natural processes might limit ice-sheet deterioration? 4. Are there human interventions that could enhance these natural processes, thereby slowing sea-level rise? 5. What is our window of opportunity for implementing these interventions? This White Paper by Professor John Moore, UArctic (University of the Arctic) of Lapland, professor Douglas MacAyeal, University of Chicago, Brent Minchew Massachusetts Institute of Technology and Michael Wolovick discuss these questions.

Glacial Climate Intervention: A Research Vision

Glacial Climate Intervention: A Research Vision

climateengineering.uchicago.edu

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