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4 June 2026 - 4 June 2026

10:00AM - 11:00AM

W309 Geography West

  • Free

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Observations show that Antarctica’s ice sheet is experiencing significant mass loss characterized by substantial interannual to decadal variability linked to large-scale climate modes like ENSO, the Southern Annular Mode, and the Amundsen Sea Low. The long-term observational record, combined with ice-sheet inertia, now holds predictive power for assessing Antarctica’s contribution to future sea-level rise.

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Observations of Antarctica’s ice sheet show clear overall mass loss, but with substantial interannual to decadal variability. This seminar will focus on:

  1. the connection of this variability to large-scale modes of climate variability — namely ENSO, the Southern Annular Mode, and the Amundsen Sea Low — demonstrating that these modes explain a significant component of the decadal variation in ice-sheet mass and elevation; and
  2. the observational record of mass change, which is now sufficiently long that, combined with assumptions about ice-sheet inertia, it may hold predictive power for Antarctica’s contribution to sea-level rise over the coming decades.

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