UNDERSTANDING SURFACE-TO-BED MELTWATER PATHWAYS ACROSS THE GREENLAND ICE SHEET USING MACHINE-LEARNING AND PHYSICS-BASED MODELS
Jointly supported by the US NSF and UK NERC, this project will begin in September 2023 and aims to better understand surface-to-bed meltwater pathways across the entire Greenland Ice Sheet using machine-learning and physics-based models. The three-year project will use a combination of remote-sensing observations, deep learning, and physics-based models with aims to: (1) detect continent-wide surface fractures, moulins and supraglacial lake drainage events within satellite imagery; (2) determine the ice-sheet conditions required to trigger supraglacial lake drainage via hydrofracture; and (3) model the impact of supraglacial lake drainage events on ice-flow dynamics at a regional scale. Lead by Prof. Ching-Yao Lai (Princeton U.), additional collaborators include Profs. Leigh Stearns (U. Kansas) and Ian Hewitt (U. Oxford Mathematical Institute). Previous work that motivates this proposal is published in Lai et al. (2021) and Stevens et al. (2015; 2018) listed below.
GREENLAND ICE SHEET DYNAMIC RESPONSE TO THE INLAND EXPANSION OF A HYDROLOGICALLY ACTIVE ICE-SHEET BED.
This project combines on-ice geodetic and radar observations with geophysical inverse and forward modeling techniques to investigate stress transmission between neighboring supraglacial lakes and moulins on the western margin of the Greenland Ice Sheet. Field observations of ice-sheet surface and englacial deformation will be collected over a 16-month period from May 2022 through August 2023. Collaborators include Drs. Meredith Nettles and Stacy Larochelle (Columbia University) and Marianne Okal (UNAVCO, Inc.).
ANTARCTIC ICE-SHELF INSTABILITY CAUSED BY ACTIVE SURFACE MELTWATER PRODUCTION, MOVEMENT, PONDING, AND HYDRO-FRACTURE.
Funded by NSFGEO–NERC, this project combines field observations, numerical modeling, and remote sensing techniques to better understand ice-shelf flexure and fracture due to surface meltwater loading. Field observations of ice-shelf surface height, local weather conditions, and water body depths are currently being collected on the George VIth Ice Shelf, Antarctic Peninsula through February 2023. This project is jointly supported by the US NSF and UK NERC, with field support provided by the British Antarctic Survey in coordination with the United States Antarctic Program. Collaborators include Drs. Alison Banwell (University of Colorado Boulder), Rebecca Dell (University of Cambridge), Douglas MacAyeal (University of Chicago), and Ian Willis (University of Cambridge).