2023-2024 USAP Field Season
Unpinning of the Ross Ice Shelf from Ross Bank
Dr. Philip Bart
Supporting Stations: RV/IB Nathaniel B. Palmer
This team will investigate the how, why and when the Ross Ice Shelf (RIS) unpinned from Ross Bank to assess ice sheet and ice shelf behavior during a recent unpinning event. Previous studies have estimated the timing of West Antarctic Ice Sheet flow changes that occurred during the past millennia based on changes in the pattern of flow stripes and rift tracks preserved on the RIS. Ongoing studies of a recently completed ice core by the Roosevelt Island Climate Evolution project are likely to provide a high-resolution record of atmospheric and ice-surface elevation changes. It is equally important to understanding the past ice shelf dynamics around Ross Bank, an essential part for determining the past behavior of RIS and the future susceptibility and response of unpinning. As such, the Ross Bank study will provide some of the needed ground truth proof for any physical or numerical model prediction of cause-and-effect relationships associated with ice-shelf unpinning. In addition to the scientific broader impacts on ice sheet dynamics and sea level rise, this study provides the opportunity to train four graduate and four undergraduate students on geophysical and geological data acquisition, processing, sampling, interpretation and presentation.
Field Season Overview
The thirteen-person science team will deploy to the Ross Bank and Pennell Basin areas on the RVIB Nathaniel B. Palmer (NBP). They will embark the vessel at McMurdo Station in February, and return to Lyttelton, New Zealand. In 2023-24, efforts will focus on sampling from selected stations at Ross Bank for sedimentary, diatom, and in situ benthic foraminifera analyses. The team will collect sediment using the Piston Corer, Jumbo Piston Corer, Box Corer, Mega Corer, Smith-MacIntyre grab, and Epibenthic Sled. Seafloor imagery via the Yo-Yo Camera and companion baseline water-column analyses with CTDs (Connectivity, Temperature, and Depth) and plankton tows will be co-acquired. Sediment cores will be shipped back to the core repository in Oregon.
Deploying Team Members