The Cryosphere, 12, 205–225, 2018 https://doi.org/10.5194/tc-12-205-2018 © Author(s) 2018. This work is distributed under the Creative Commons Attribution 4.0 License. Seafloor geomorphology of western Antarctic Peninsula bays: a signature of ice flow behaviour Yuribia P. Munoz and Julia S. Wellner Department of Earth and Atmospheric Sciences, University of Houston, Houston, Texas 77204, USA Correspondence: Yuribia P. Munoz (
[email protected]) Received: 12 June 2017 – Discussion started: 22 June 2017 Revised: 4 November 2017 – Accepted: 13 November 2017 – Published: 22 January 2018 Abstract. Glacial geomorphology is used in Antarctica to 1 Introduction reconstruct ice advance during the Last Glacial Maximum and subsequent retreat across the continental shelf. Analo- While warming temperatures in the Antarctic Peninsula (AP) gous geomorphic assemblages are found in glaciated fjords have resulted in the retreat of 90 % of the regional glaciers and are used to interpret the glacial history and glacial dy- (Cook et al., 2014) and the collapse of ice shelves (Morris namics in those areas. In addition, understanding the distri- and Vaughan, 2003; Cook and Vaughan, 2010), recent stud- bution of submarine landforms in bays and the local con- ies have shown that since the late 1990s this region is cur- trols exerted on ice flow can help improve numerical models rently experiencing a cooling trend (Turner et al., 2016). The by providing constraints through these drainage areas. We AP is a dynamic region that serves as a natural laboratory present multibeam swath bathymetry from several bays in to study ice flow and the resulting sediment deposits.