Open Access Repository

Cold ocean cavity and weak basal melting of the Sorsdal Ice Shelf revealed by surveys using autonomous platforms


Downloads per month over past year

Gwyther, DE ORCID: 0000-0002-7218-2785, Spain, EA, King, P ORCID: 0000-0001-9436-0936, Guihen, D ORCID: 0000-0002-5786-6599, Williams, GD ORCID: 0000-0003-1769-8356, Evans, E ORCID: 0000-0003-2393-4271, Cook, S ORCID: 0000-0001-9878-4218, Richter, O ORCID: 0000-0002-5857-8361, Galton-Fenzi, BK and Coleman, R ORCID: 0000-0002-9731-7498 2020 , 'Cold ocean cavity and weak basal melting of the Sorsdal Ice Shelf revealed by surveys using autonomous platforms' , JGR Oceans, vol. 125, no. 6 , pp. 1-17 , doi: 10.1029/2019JC015882.

139536 - Cold o...pdf | Download (7MB)

| Preview


Basal melting of ice shelves is inherently difficult to quantify through direct observations, yet it is a critical factor controlling Antarctic mass balance and global sea‐level rise. While much research attention is paid to larger ice shelves and those experiencing the most rapid change, many smaller, unstudied ice shelves offer valuable insights. Here, we investigate the oceanographic conditions and melting beneath the Sørsdal ice shelf, East Antarctica. We present results from the 2018/2019 Sørsdal deployment of the University of Tasmania's autonomous underwater vehicle nupiri muka . Oceanography adjacent to and beneath the ice shelf front shows a cold and relatively saline environment dominated by Winter Water and Dense Shelf Water, while bathymetry measurements show a deep (∼1,200 m) trough running into the ice shelf cavity. Two multiyear deployments of Autonomous Phase‐sensitive Radar Echo Sounders on the surface of the ice shelf show weak melt rates (average of 1.6 and 2.3 m yr−1) with low temporal variability. These observations are supported by numerical ocean model and satellite estimates of melting. We speculate that the presence of a ∼825 m thick (350 m to at least 1,175 m) homogeneous layer of cold, dense water blocks access from warmer waters that intrude into Prydz Bay from offshore, resulting in weak melt rates. However, the newly identified trough means that the ice shelf is vulnerable to any decrease in polynya activity that allows warm water to enter the cavity. This could lead to increased basal melting and mass loss through this sector of Antarctica.

Item Type: Article
Authors/Creators:Gwyther, DE and Spain, EA and King, P and Guihen, D and Williams, GD and Evans, E and Cook, S and Richter, O and Galton-Fenzi, BK and Coleman, R
Keywords: Antarctica, ice shelves, AUV, oceanography
Journal or Publication Title: JGR Oceans
Publisher: Wiley-Blackwell Publishing Inc.
ISSN: 2169-9275
DOI / ID Number: 10.1029/2019JC015882
Copyright Information:

Copyright 2020 The Authors. Licensed under Creative Commons Attribution 4.0 International (CC BY 4.0)

Related URLs:
Item Statistics: View statistics for this item

Actions (login required)

Item Control Page Item Control Page