Rapid drilling to find ancient ice
A new drill (the Rapid Access Isotope Drill, or RAID) is being developed by BAS which, rather than collect a full ice-core, this drill will chop up the ice and will allow collecting ice chippings.
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A new drill (the Rapid Access Isotope Drill, or RAID) is being developed by BAS which, rather than collect a full ice-core, this drill will chop up the ice and will allow collecting ice chippings.
By exploiting advances in ice sheet modelling, and new Antarctic-wide datasets, this project aims to predict how far and how fast the observed ocean-driven thinning of floating ice shelves will propagate into the interior of the Antarctic ice sheet, and assess the consequences for global sea level over decadal-to-centennial timescales.
The ice sheet modelling group integrates observational data with dynamical models to improve our representation of how the ice flows beneath the surface, and to reveal how the shape and flow of the Antarctic ice sheet has changed in the past.
This project used ice cores drilled across the Antarctic Peninsula and West Antarctica to reconstruct past climate and understand whether the recent warming in these rapidly changing regions is unusual over longer timescales..
This project studies the last Interglacial (129-116 thousand years ago, ka) when CO2 and global temperature were both higher than they were before human industrialisation. By examining Last Interglacial climate, we can gain insights into climate processes and feedbacks close to those expected by the end of the 21st century.
A project studying the impact of ocean acidification on pteropods, small shelled marine animals considered a sentinel species for ocean acidification.
This research aims to improve estimates of Antarctica’s contribution to sea level. Sea level is currently rising at approximately 3mm/yr.
Why does global biodiversity show such a steep increase just as climates were deteriorating?
This project used ice core chemical and biological tracers, including marine diatoms swept onto the ice sheet by wind, to reconstruct 300 years of wind strength and atmospheric circulation patterns in West Antarctica.
This research focuses on investigating the glacial histories of Arctic ice sheets and ice caps using the marine geological record preserved on continental margins.
In this NERC-funded project, we are generating Southern Hemisphere Westerlies (SHW) proxy records from each of the three major sectors of the Southern Ocean, focusing on subantarctic islands situated in the core belt of the SHW.
During this project essential survey data was collected to help plan future deep ocean drilling expeditions.