Article

 

Direct measurements of ice-shelf flexure caused by surface meltwater ponding and drainage Público Deposited

Conteúdo disponível para baixar

Baixar PDF
https://scholar.colorado.edu/concern/articles/2z10wr136
Abstract
  • Global sea-level rise is caused, in part, by more rapid ice discharge from Antarctica, following the removal of the restraining forces of floating ice-shelves after their break-up. A trigger of ice-shelf break-up is thought to be stress variations associated with surface meltwater ponding and drainage, causing flexure and fracture. But until now, there have been no direct measurements of these processes. Here, we present field data from the McMurdo Ice Shelf, Antarctica, showing that the filling, to ~2 m depth, and subsequent draining, by overflow and channel incision, of four surface lakes causes pronounced and immediate ice-shelf flexure over multiple-week timescales. The magnitude of the vertical ice-shelf deflection reaches maxima of ~1 m at the lake centres, declining to zero at distances ofmodels, which currently do not simulate ice-shelf break-up due to meltwater loading and unloading.
Creator
Date Issued
  • 2019-02-13
Academic Affiliation
Journal Title
Journal Volume
  • 10
Última modificação
  • 2019-12-09
Resource Type
Declaração de direitos
DOI
ISSN
  • 2041-1723
Language

Relações

Itens