Glaciers offer the potential to reconstruct past climate over timescales from decades to
millennia. They are found on nearly every continent, and at the Last Glacial Maximum …

Numerical glacier models applied to moraine chronologies provide an opportunity to
quantify past climate change. Here we apply a two-dimensional coupled mass balance–ice …

Glaciers reflect integrated climate signals from inter-annual to centennial timescales. In
using glacier extent as a climate-change detector, the challenge is to distinguish the roles of …

Inter-annual climate variability has the potential to induce hundred-to-thousand meters of
glacier length change, comparable to the glacier retreats from their Little Ice Age (LIA) …

Determining what caused the global Last Glaciation and last glacial termination, despite
opposing orbital summer insolation signatures between the polar hemispheres, remains a …

Glaciers fluctuate in response to climate change and record these changes by building
sedimentary landforms, including moraines. Therefore, glacial landscapes are a potentially …

It is standard to compare climate model results covering the past millennium and
reconstructions based on various archives in order to test the ability of models to reproduce …

The magnitude of tropical cooling during the Last Glacial Maximum (LGM;∼ 19–26.5 ka)
remains controversial, with sea‐surface temperatures cooling by several degrees less than …

Geological records of past glacier extent can yield important constraints on the timing and
magnitude of pre-historic climate change. Here we present a cosmogenic 3 He moraine …

Abstract The Last Glacial-Interglacial Transition (LGIT) was a dynamic stage of Earth's
history, and the difficulty of reconstructing this complex interval may be compounded by …