Articles | Volume 14, issue 9 
            
                
                    
            
            
            https://doi.org/10.5194/tc-14-2883-2020
                    © Author(s) 2020. This work is distributed under 
the Creative Commons Attribution 4.0 License.
                the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/tc-14-2883-2020
                    © Author(s) 2020. This work is distributed under 
the Creative Commons Attribution 4.0 License.
                the Creative Commons Attribution 4.0 License.
Revealing the former bed of Thwaites Glacier using sea-floor bathymetry: implications for warm-water routing and bed controls on ice flow and buttressing
                                            British Antarctic Survey, Natural Environment Research Council,
High Cross, Madingley Road, Cambridge, CB3 0ET, UK
                                        
                                    Robert D. Larter
                                            British Antarctic Survey, Natural Environment Research Council,
High Cross, Madingley Road, Cambridge, CB3 0ET, UK
                                        
                                    Alastair G. C. Graham
                                            College of
Marine Science, University of South Florida, Saint Petersburg, FL 33701, USA
                                        
                                    Robert Arthern
                                            British Antarctic Survey, Natural Environment Research Council,
High Cross, Madingley Road, Cambridge, CB3 0ET, UK
                                        
                                    James D. Kirkham
                                            British Antarctic Survey, Natural Environment Research Council,
High Cross, Madingley Road, Cambridge, CB3 0ET, UK
                                        
                                    
                                            Scott Polar Research Institute, University of Cambridge, Lensfield
Road, Cambridge, CB2 1ER, UK
                                        
                                    Rebecca L. Totten
                                            Department of Geological Sciences, University of Alabama, Tuscaloosa,
AL 35487, USA
                                        
                                    Tom A. Jordan
                                            British Antarctic Survey, Natural Environment Research Council,
High Cross, Madingley Road, Cambridge, CB3 0ET, UK
                                        
                                    Rachel Clark
                                            Department of Earth and Atmospheric Sciences, University of Houston,
Houston, TX 77204, USA
                                        
                                    Victoria Fitzgerald
                                            Department of Geological Sciences, University of Alabama, Tuscaloosa,
AL 35487, USA
                                        
                                    Anna K. Wåhlin
                                            Department of Marine Sciences, University of Gothenburg, 40530
Göteborg, Sweden
                                        
                                    John B. Anderson
                                            Department of Earth Science, Rice University, Houston, TX 77005, USA
                                        
                                    Claus-Dieter Hillenbrand
                                            British Antarctic Survey, Natural Environment Research Council,
High Cross, Madingley Road, Cambridge, CB3 0ET, UK
                                        
                                    Frank O. Nitsche
                                            Lamont-Doherty Earth Observatory, Columbia University, Palisades, New
York, NY, USA
                                        
                                    Lauren Simkins
                                            Department of Environmental Sciences, University of Virginia,
Charlottesville, VA 22904, USA
                                        
                                    James A. Smith
                                            British Antarctic Survey, Natural Environment Research Council,
High Cross, Madingley Road, Cambridge, CB3 0ET, UK
                                        
                                    Karsten Gohl
                                            Alfred Wegener Institute Helmholtz-Centre for Polar and Marine
Research, 27568 Bremerhaven, Germany
                                        
                                    Jan Erik Arndt
                                            Alfred Wegener Institute Helmholtz-Centre for Polar and Marine
Research, 27568 Bremerhaven, Germany
                                        
                                    Jongkuk Hong
                                            Korea Polar Research Institute (KOPRI), Incheon 21990, Republic of
Korea
                                        
                                    Julia Wellner
                                            Department of Earth and Atmospheric Sciences, University of Houston,
Houston, TX 77204, USA
                                        
                                    Data sets
A multibeam-bathymetric compilation for the southern Amundsen Sea shelf, 1999--2019 (Version 1.0) K. A. Hogan, R. D. Larter, A. G. C. Graham, F. O. Nitsche, J. D. Kirkham, R. Totten Minzoni, R. Clark, V. Fitzgerald, J. B. Anderson, C.-D. Hillenbrand, L. Simkins, J. A. Smith, K. Gohl, J. E. Arndt, J. Hong, K. J. Heywood, E. P. Abrahamsen, A. F. Thompson, R. Dunbar, and J. S. Wellner https://doi.org/10.5285/F2DFEDA9-BF44-4EF5-89A3-EE5E434A385C
Short summary
            The sea-floor geometry around the rapidly changing Thwaites Glacier is a key control on warm ocean waters reaching the ice shelf and grounding zone beyond. This area was previously unsurveyed due to icebergs and sea-ice cover. The International Thwaites Glacier Collaboration mapped this area for the first time in 2019. The data reveal troughs over 1200 m deep and, as this region is thought to have only ungrounded recently, provide key insights into the morphology beneath the grounded ice sheet.
            The sea-floor geometry around the rapidly changing Thwaites Glacier is a key control on warm...
            
         
 
             
             
             
            