Joughin, IanShapero, DanielDutrieux, PierreSmith, Ben2021-03-042021-03-042021-03-01http://hdl.handle.net/1773/46687Speedup of Pine Island Glacier over the last several decades has made it Antarctica’s largest contributor to sea-level rise. The past speedup is largely due to grounding-line retreat in response to ocean-induced thinning that reduced ice-shelf buttressing. These data are the model inputs and other observations associated with two papers that use an ice-flow model to investigate recent speedup of Pine Island Glacier, along with how continued melting may affect the glacier over the next 200 year.Attribution 3.0 United Stateshttp://creativecommons.org/licenses/by/3.0/us/Dataset