adamsgaard.dk

my academic webpage
git clone git://src.adamsgaard.dk/adamsgaard.dk # fast
git clone https://src.adamsgaard.dk/adamsgaard.dk.git # slow
Log | Files | Refs | README | LICENSE Back to index

012-agu2021.txt (2031B)


      1 Below is my recorded talk for the [1]American Geophysical Union 2021 Fall
      2 Meeting. Full abstract:
      3 
      4     Title: Process-based modeling of glacial till advection
      5 
      6     Anders Damsgaard(1), Jan A. Piotrowski(1), Ian Madden(2), Jenny Suckale(2),
      7     Kenny K. Sørensen(3)
      8 
      9     1: Department of Geoscience, Aarhus University, Denmark
     10     2: Department of Geophysics, Stanford University, CA, USA
     11     3: Department of Civil and Architectural Engineering, Aarhus University,
     12     Denmark
     13 
     14     Glacial flow can reshape the Earth surface through erosion and deposition.
     15     Many past and present ice sheets lie on soft beds, and till mobilization
     16     and transport is governed by the degree of basal coupling, fluctuations in
     17     thermal state, subglacial hydrology, and the mechanics of the basal till
     18     itself. Changes in basal topography due to ice movement could theoretically
     19     feed back onto ice-flow dynamics. For example, the buildup of sedimentary
     20     grounding-zone wedges at the marine termini of ice streams may stabilize
     21     their position against local sea-level change. However, modeling of
     22     subglacial till advection has previously relied on fluid-like rheologies,
     23     which contrasts the now established concensus of Mohr-Coulomb plasticity.
     24 
     25     In our work, we aim to improve the parameterization of till advection by
     26     glacial flow. We compare a new continuum model for till against laboratory
     27     consolidation and ring-shear experiments. We show how transient dynamics in
     28     porosity and strength affect the mechanics under non-steady forcings, such
     29     as glacier stick-slip or surge. We couple the till continuum model to an
     30     ice-stream model, and demonstrate how till transport varies when ice flows
     31     over simple soft-bed basal geometries, and affects ice-stream sensitivity
     32     to external forcings.
     33 
     34 Slides and video:
     35 
     36     - slides: gopher://adamsgaard.dk/9/npub/agu2021-damsgaard.pdf
     37     - video: https://adamsgaard.dk/video/agu2021-damsgaard.mp4
     38 
     39 References:
     40 
     41 [1] https://www.agu.org/Fall-Meeting
     42