Growth and retreat of the last British–Irish Ice Sheet, 31 000 to 15 000 years ago: the BRITICE‐CHRONO reconstruction

Chris D. Clark, Jeremy C. Ely, Richard C. A. Hindmarsh, +35

Boreas

EngineeringGeomorphologySecond Order ControlsArchaeologyGlacial Process +14

Proglacial Lakes Control Glacier Geometry and Behavior During Recession

Jenna L. Sutherland, Jonathan L. Carrivick, Niall Gandy, +3

Geophysical Research Letters

GlacierEngineeringGeomorphologyClimate ModelingGlacial Process +14

Exploring the ingredients required to successfully model the placement, generation, and evolution of ice streams in the British-Irish Ice Sheet

Niall Gandy, Lauren Gregoire, Jeremy C. Ely, +3

Quaternary Science Reviews

Recent progress on combining geomorphological and geochronological data with ice sheet modelling, demonstrated using the last British–Irish Ice Sheet

Jeremy C. Ely, Chris D. Clark, Richard C. A. Hindmarsh, +8

Journal of Quaternary Science

Empirical ReconstructionsGlacierIce Sheet ExtentEngineeringGeomorphology +14

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

Niall Gandy, Lauren Gregoire, Jeremy C. Ely, +3

Journal of Geophysical Research Earth Surface

EngineeringGeomorphologyIce FlowSurface MeltOceanography +17

Marine ice sheet instability and ice shelf buttressing of the Minch Ice Stream, northwest Scotland

Niall Gandy, Lauren Gregoire, Jeremy C. Ely, +5

˜The œcryosphere

Minch Ice StreamEngineeringGeomorphologyClimate ModelingOceanography +19

The collapse of the Cordilleran–Laurentide ice saddle and early opening of the Mackenzie Valley, Northwest Territories, Canada, constrained by ¹⁰ Be exposure dating

Benjamin J. Stoker, Martin Margold, John Gosse, +7

˜The œcryosphere

De‐Tuning Albedo Parameters in a Coupled Climate Ice Sheet Model to Simulate the North American Ice Sheet at the Last Glacial Maximum

Niall Gandy, Lachlan Astfalck, Lauren Gregoire, +6

Journal of Geophysical Research Earth Surface

GlacierIce Sheet ExtentEngineeringClimate ModelingLast Glacial Maximum +17