The present interglacial, the Holocene, spans the period of the last 11,700 years. It has
sustained the growth and development of modern society. The millennial-scale decreasing …

A global overview of glacier advances and retreats (grouped by regions and by millennia)
for the Holocene is compiled from previous studies. The reconstructions of glacier …

Past deglacial ice sheet reconstructions have generally relied upon discipline-specific
constraints with no attention given to the determination of objective confidence intervals …

This synthesis paper summarizes published proxy climate evidence showing the spatial and
temporal pattern of climate change through the Holocene in Arctic Canada and Greenland …

The most recent deglaciation of the North American Ice Sheet Complex (NAISC: comprising
the Innuitian, Cordilleran, and Laurentide ice sheets) offers a broad perspective from which …

Multiproxy climate records from Iceland document complex changes in terrestrial climate
and glacier fluctuations through the Holocene, revealing some coherent patterns of change …

Understanding patterns of ice-sheet deglaciation is key for predicting the rate of future ice-
sheet melt, yet the processes underlying deglaciation remain elusive. The early Holocene …

Several global and regional factors contribute to observed sea-level change along any
particular coast. Global processes include changes in ocean mass (glacio-eustasy from ice …

For more than four decades, the reporting of 14C dates on marine molluscs from Arctic
Canada has been notable for the lack of consistently applied marine reservoir corrections …

Alpine glacier fluctuations provide important paleoclimate proxies where other records such
as ice cores, tree rings, and speleothems are not available. About 20 years have passed …