[HTML][HTML] Deglaciation of the Eurasian ice sheet complex
The Eurasian ice sheet complex (EISC) was the third largest ice mass during the Last
Glacial Maximum with a span of over 4500 km and responsible for around 20 m of eustatic …
Glacial Maximum with a span of over 4500 km and responsible for around 20 m of eustatic …
A spatially-restricted Younger Dryas plateau icefield in the Gaick, Scotland: Reconstruction and palaeoclimatic implications
Considerable research has been conducted in Scotland to reconstruct Younger Dryas
glaciers and palaeoclimatic conditions, but our understanding remains incomplete. In this …
glaciers and palaeoclimatic conditions, but our understanding remains incomplete. In this …
A tool for the ages: the probabilistic cosmogenic age analysis tool (P-CAAT)
While revolutionary to the geomorphic community, the application of terrestrial cosmogenic
nuclide (TCN) dating is complicated by geological uncertainties, which often lead to skewed …
nuclide (TCN) dating is complicated by geological uncertainties, which often lead to skewed …
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 …
Atlantic Water advection vs. glacier dynamics in northern Spitsbergen since early deglaciation
Atlantic Water (AW) advection plays an important role in climatic, oceanographic and
environmental conditions in the eastern Arctic. Situated along the only deep connection …
environmental conditions in the eastern Arctic. Situated along the only deep connection …
[HTML][HTML] A revised chronology for the growth and demise of Loch Lomond Readvance ('Younger Dryas') ice lobes in the Lochaber area, Scotland
We present a revised varve chronology for the duration of ice-dammed lakes that formed in
the Lochaber district, Scotland, during the Loch Lomond ('Younger Dryas') Stadial. We …
the Lochaber district, Scotland, during the Loch Lomond ('Younger Dryas') Stadial. We …
The glacial geomorphology of the Loch Lomond (Younger Dryas) Stadial in Britain: a review
This paper systematically reviews the glacial geomorphological evidence of the Loch
Lomond Stadial (LLS; Younger Dryas) glaciation in Britain (12.9–11.7 ka). The …
Lomond Stadial (LLS; Younger Dryas) glaciation in Britain (12.9–11.7 ka). The …
On the timing of retreat of the Loch Lomond ('Younger Dryas') Readvance icefield in the SW Scottish Highlands and its wider significance
It has long been assumed that the last glacier expansion in the Scottish Highlands, the Loch
Lomond Readvance (LLR), resulted from a cold reversal that was broadly coeval with the …
Lomond Readvance (LLR), resulted from a cold reversal that was broadly coeval with the …
[HTML][HTML] Trough geometry was a greater influence than climate-ocean forcing in regulating retreat of the marine-based Irish-Sea Ice Stream
Marine terminating ice streams are a major component of contemporary ice sheets and are
likely to have a fundamental influence on their future evolution and concomitant contribution …
likely to have a fundamental influence on their future evolution and concomitant contribution …
Glacial landsystems, retreat dynamics and controls on Loch Lomond Stadial (Younger Dryas) glaciation in Britain
Glacial geomorphology relating to the Loch Lomond Stadial (Younger Dryas) in Britain is
used to construct five glacial landsystem models. These landsystems lie on a continuum of …
used to construct five glacial landsystem models. These landsystems lie on a continuum of …