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] 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 …
Retreat and stabilization of a marine-based ice margin along a high arctic fjord-cross-shelf trough system
PO Couette, P Lajeunesse, JF Ghienne… - Quaternary Science …, 2023 - Elsevier
Multibeam bathymetric and seismostratigraphic data collected in the Clyde fjord-cross-shelf
trough system (eastern Baffin Island, Canadian Arctic Archipelago) display glacial landforms …
trough system (eastern Baffin Island, Canadian Arctic Archipelago) display glacial landforms …
The North Atlantic Glacial Eastern Boundary Current as a key driver for ice‐sheet—AMOC interactions and climate instability
The upper branch of the Atlantic meridional overturning circulation (AMOC) plays a critical
role in ocean circulation and climate change, yet its variability during the last glacial period …
role in ocean circulation and climate change, yet its variability during the last glacial period …
Marine isotope stage 4 (71–57 ka) on the Western European margin: insights to the drainage and dynamics of the Western European Ice Sheet
Abstract Marine Isotope Stage (MIS) 4 (ca. 71–57 ka; within the Middle Weichselian
Substage) is considered a significant Pleistocene glaciation, but it remains poorly …
Substage) is considered a significant Pleistocene glaciation, but it remains poorly …
The geomorphology of Ireland's continental shelf
ABSTRACT The Irish Shelf Seabed Geomorphological Map (ISSGM)(v2023) presented
here, is the first high-resolution geomorphological map of the entire Irish continental shelf …
here, is the first high-resolution geomorphological map of the entire Irish continental shelf …
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 …
The evolution of the terrestrial‐terminating Irish Sea glacier during the last glaciation
RC Chiverrell, GSP Thomas, M Burke… - Journal of …, 2021 - Wiley Online Library
Here we reconstruct the last advance to maximum limits and retreat of the Irish Sea Glacier
(ISG), the only land‐terminating ice lobe of the western British Irish Ice Sheet. A series of …
(ISG), the only land‐terminating ice lobe of the western British Irish Ice Sheet. A series of …
Collapse of the last Eurasian Ice Sheet in the North Sea modulated by combined processes of ice flow, surface melt, and marine ice sheet instabilities
The record of the confluence and collapse of the British‐Irish Ice Sheet and the
Fennoscandian Ice Sheet is obscured by the North Sea, hindering reconstructions of the …
Fennoscandian Ice Sheet is obscured by the North Sea, hindering reconstructions of the …
Pattern, style and timing of British–Irish Ice Sheet retreat: Shetland and northern North Sea sector
The offshore sector around Shetland remains one of the least well‐studied parts of the
former British–Irish Ice Sheet with several long‐standing scientific issues unresolved. These …
former British–Irish Ice Sheet with several long‐standing scientific issues unresolved. These …