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Relative sea-level changes and crustal movements in Britain and Ireland since the Last Glacial Maximum
The new sea-level database for Britain and Ireland contains> 2100 data points from 86
regions and records relative sea-level (RSL) changes over the last 20 ka and across …
regions and records relative sea-level (RSL) changes over the last 20 ka and across …
Growth and retreat of the last British–Irish Ice Sheet, 31 000 to 15 000 years ago: the BRITICE‐CHRONO reconstruction
The BRITICE‐CHRONO consortium of researchers undertook a dating programme to
constrain the timing of advance, maximum extent and retreat of the British–Irish Ice Sheet …
constrain the timing of advance, maximum extent and retreat of the British–Irish Ice Sheet …
[HTML][HTML] Asynchronous dynamics of the last Scandinavian Ice Sheet along the Pomeranian ice-marginal belt: A new scenario inferred from surface exposure 10Be …
We present a new set of 25 10 Be surface exposure ages of boulders located on the
Pomeranian moraines and of erratic boulders located directly upstream of the Pomeranian …
Pomeranian moraines and of erratic boulders located directly upstream of the Pomeranian …
The last Scottish ice sheet
The last Scottish Ice Sheet (SIS) expanded from a pre-existing ice cap after∼ 35 ka.
Highland ice dominated, with subsequent build-up of a Southern Uplands ice mass. The …
Highland ice dominated, with subsequent build-up of a Southern Uplands ice mass. The …
Pattern, style and timing of British–Irish Ice Sheet advance and retreat over the last 45 000 years: evidence from NW Scotland and the adjacent continental shelf
Predicting the future response of ice sheets to climate warming and rising global sea level is
important but difficult. This is especially so when fast‐flowing glaciers or ice streams …
important but difficult. This is especially so when fast‐flowing glaciers or ice streams …
[HTML][HTML] Extent and retreat history of the Barra Fan Ice Stream offshore western Scotland and northern Ireland during the last glaciation
Abstract During the Last Glacial Maximum (LGM) the marine-terminating Barra Fan Ice
Stream (BFIS), a major conduit of the British Irish Ice Sheet (BIIS), drained much of western …
Stream (BFIS), a major conduit of the British Irish Ice Sheet (BIIS), drained much of western …
Exploring the ingredients required to successfully model the placement, generation, and evolution of ice streams in the British-Irish Ice Sheet
Ice stream evolution is a major uncertainty in projections of the future of the Greenland and
Antarctic Ice sheets. Accurate simulation of ice stream evolution requires an understanding …
Antarctic Ice sheets. Accurate simulation of ice stream evolution requires an understanding …
Lateglacial shifts in seasonality reconcile conflicting North Atlantic temperature signals
The accelerating flux of glacial meltwater to the oceans due to global warming is a potential
trigger for future climate disturbance. Past disruption of Atlantic Ocean circulation, driven by …
trigger for future climate disturbance. Past disruption of Atlantic Ocean circulation, driven by …
Recent progress on combining geomorphological and geochronological data with ice sheet modelling, demonstrated using the last British–Irish Ice Sheet
Palaeo‐ice sheets are important analogues for understanding contemporary ice sheets,
offering a record of ice sheet behaviour that spans millennia. There are two main …
offering a record of ice sheet behaviour that spans millennia. There are two main …
[HTML][HTML] Early deglaciation of the British-Irish Ice Sheet on the Atlantic shelf northwest of Ireland driven by glacioisostatic depression and high relative sea level
Understanding the triggers and pace of marine-based ice sheet decay is critical for
constraining the future mass loss and dynamic behaviour of marine-based sectors of the …
constraining the future mass loss and dynamic behaviour of marine-based sectors of the …