Ocean forced variability of Totten Glacier mass loss

@article{Roberts2017OceanFV,
  title={Ocean forced variability of Totten Glacier mass loss},
  author={Jason L. Roberts and Benjamin Keith Galton-Fenzi and Fernando S. Paolo and Claire Donnelly and David E. Gwyther and Laurie Padman and Duncan Young and R. C. Warner and Jamin Stevens Greenbaum and Helen Amanda Fricker and Antony J. Payne and Stephen L. Cornford and Anne M. Le Brocq and Tas D. van Ommen and Donald D. Blankenship and Martin J. Siegert},
  journal={Special Publications},
  year={2017},
  volume={461},
  pages={175 - 186}
}
Abstract A large volume of the East Antarctic Ice Sheet drains through the Totten Glacier (TG) and is thought to be a potential source of substantial global sea-level rise over the coming centuries. We show that the surface velocity and height of the floating part of the TG, which buttresses the grounded component, have varied substantially over two decades (1989–2011), with variations in surface height strongly anti-correlated with simulated basal melt rates (r = 0.70, p < 0.05). Coupled… 
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TLDR
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Seasonality of Warm Water Intrusions Onto the Continental Shelf Near the Totten Glacier
Warm Modified Circumpolar Deep Water (MCDW) from the Southern Ocean drives rapid basal melt of the Totten Ice Shelf on the Sabrina Coast (East Antarctica), affecting the mass balance of the grounded
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