DPG Phi
Verhandlungen
Verhandlungen
DPG

Rostock 2019 – wissenschaftliches Programm

Bereiche | Tage | Auswahl | Suche | Aktualisierungen | Downloads | Hilfe

AKE: Arbeitskreis Energie

AKE 13: Climate Change

AKE 13.1: Hauptvortrag

Mittwoch, 13. März 2019, 16:15–16:45, U A-Esch 1

The far reach of ice-shelf thinning in AntarcticaRonja Reese1,2, Hilmar Gudmundsson3, Anders Levermann1,2,4, and •Ricarda Winkelmann1,21Potsdam Institute for Climate Impact Research (PIK), Potsdam, Germany — 2University of Potsdam, Potsdam, Germany — 3Northumbria University, Newcastle upon Tyne, UK — 4Lamont Doherty Earth Observatory, Columbia University, New York, NY, USA

Floating ice shelves, which fringe most of Antarctica's coastline, regulate ice flow into the Southern Ocean. Their thinning or disintegration can cause upstream acceleration of grounded ice and raise global sea levels. So far the effect has not been quantified in a comprehensive and spatially explicit manner. Here, using a finite-element model, we diagnose the immediate, continent-wide flux response to different spatial patterns of ice-shelf mass loss. We show that highly localized ice-shelf thinning can reach across the entire shelf and accelerate ice flow in regions far from the initial perturbation. As an example, this tele-buttressing enhances outflow from Bindschadler Ice Stream in response to thinning near Ross Island more than 900 km away. We further find that the integrated flux response across all grounding lines is highly dependent on the location of imposed changes: the strongest response is caused not only near ice streams and ice rises, but also by thinning, for instance, well-within the Filchner-Ronne and Ross Ice Shelves. The most critical regions in all major ice shelves are often located in regions easily accessible to the intrusion of warm ocean waters, stressing Antarctica's vulnerability to changes in its surrounding ocean.

100% | Mobil-Ansicht | English Version | Kontakt/Impressum/Datenschutz
DPG-Physik > DPG-Verhandlungen > 2019 > Rostock