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Articles by Michael Bevis
Transient ice loss in the Patagonia Icefields during the 2015–2016 El Niño event - Scientific Reports
Abstract The Patagonia Icefields (PIF) are the largest non-polar ice mass in the southern hemisphere. The icefields cover an area of approximately 16,500 km2 and are divided into the northern and southern icefields, which are ~ 4000 km2 and ~ 12,500 km2, respectively. While both icefields have been losing mass rapidly, their responsiveness to various climate drivers, such as the El Niño-Southern Oscillation, is not well understood.
Roundup Top 10!
9/27/19 Roundup tags: Roundup Top 10 Video of the Week Video of the Week: The Historical Context of Impeachment For the fourth time in American history, an impeachment inquiry has been launched against a sitting president. Presidential historian Jon Meacham joins Chris Jansing to discuss the context of this monumental moment in time. Roundup Top 10 comments powered by
How Understanding the History of the Earth's Climate Can Offer Hope Amid Crisis
There is no longer any debate that global warming is real, and that it is happening now at an alarming rate. It is transforming the global climate system before our eyes. The rise of fossil-fueled economies over the past 200 years, and especially the accelerating CO2 emissions since the end of World War II, is clearly the cause of our mounting climate crisis. But even though 99% of climate scientists recognize what is happening, it can still be difficult to grasp something of such magnitude.
Accelerating changes in ice mass within Greenland, and the ice sheet’s sensitivity to atmospheric forcing
Significance The recent deglaciation of Greenland is a response to both oceanic and atmospheric forcings. From 2000 to 2010, ice loss was concentrated in the southeast and northwest margins of the ice sheet, in large part due to the increasing discharge of marine-terminating outlet glaciers, emphasizing the importance of oceanic forcing.
Observed rapid bedrock uplift in Amundsen Sea Embayment promotes ice-sheet stability
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The influence of gravity on the displacement field produced by fault slip
We calculated surface displacements produced by a synthetic megathrust earthquake using two spherical, layered, elastic dislocation models which differ only in that one model accounts for the coupling between elasticity and gravity and the other does not. We show that including gravity perturbs the displacement field differently in the near-, medium- and far-fields.
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