IMIS

Publications | Institutes | Persons | Datasets | Projects | Maps | Infrastructure
[ report an error in this record ]basket (0): add | show Print this page

Delicate seafloor landforms reveal past Antarctic grounding-line retreat of kilometers per year
Dowdeswell, J.A.; Batchelor, C.L.; Montelli, A.; Ottesen, D.; Christie, F.D.W.; Dowdeswell, E.K.; Evans, J. (2020). Delicate seafloor landforms reveal past Antarctic grounding-line retreat of kilometers per year. Science (Wash.) 368(6494): 1020-1024. https://dx.doi.org/10.1126/science.aaz3059
In: Science (Washington). American Association for the Advancement of Science: New York, N.Y. ISSN 0036-8075; e-ISSN 1095-9203, more
Peer reviewed article  

Available in  Authors 

Authors  Top 
  • Dowdeswell, J.A.
  • Batchelor, C.L.
  • Montelli, A.
  • Ottesen, D.
  • Christie, F.D.W.
  • Dowdeswell, E.K.
  • Evans, J.

Abstract
    A suite of grounding-line landforms on the Antarctic seafloor, imaged at submeter horizontal resolution from an autonomous underwater vehicle, enables calculation of ice sheet retreat rates from a complex of grounding-zone wedges on the Larsen continental shelf, western Weddell Sea. The landforms are delicate sets of up to 90 ridges, <1.5 meters high and spaced 20 to 25 meters apart. We interpret these ridges as the product of squeezing up of soft sediment during the rise and fall of the retreating ice sheet grounding line during successive tidal cycles. Grounding-line retreat rates of 40 to 50 meters per day (>10 kilometers per year) are inferred during regional deglaciation of the Larsen shelf. If repeated today, such rapid mass loss to the ocean would have clear implications for increasing the rate of global sea level rise.

All data in the Integrated Marine Information System (IMIS) is subject to the VLIZ privacy policy Top | Authors