Observed changes and impacts Ongoing climate trends have exacerbated many extreme
events (very high confidence). The Australian trends include further warming and sea level …

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 …

The sparsity of high-resolution 10 Be chronologies in the Northern Hemisphere makes it
difficult to determine whether the global fluctuations in glacier extent during the last glacial …

An end of summer snowline (EOSS) photographic dataset for Aotearoa New Zealand
contains over four decades of equilibrium line altitude (ELA) observations for more than 50 …

Global glacier mass loss is causing expansion of proglacial landscapes and producing
meltwater that can become impounded as lakes within natural topographic depressions or …

Glacierized mountain ranges such as the Himalaya comprise a variety of glacier types,
including clean and debris-covered glaciers. Monitoring their behaviour over time requires …

Alongside growing awareness of the significance of environmental change for glacier
regions, and their tourism-dependent communities, is the realization of the need to adapt to …

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 …

Glaciers in Afghanistan are crucial elements for water resource and summer river flows.
They are also threatened by rapid climate warming. This study presents an up-to-date …

Landslide deposits preserved in the geological record afford opportunities to better inform
hillslope and seismic hazard and risk models, particularly in regions where observational …