The oscillations between glacial and interglacial climate conditions over the past three
million years have been characterized by a transfer of immense amounts of water between …

Abstract The Laurentide Ice Sheet was the largest global ice mass to grow and decay during
the last glacial cycle (~ 115 ka to~ 10 ka). Despite its importance for driving major changes …

This third edition of Reconstructing Quaternary Environments has been completely revised
and updated to provide a new account of the history and scale of environmental changes …

Large ice sheets actively interact with the rest of the climate system by amplifying, pacing,
and potentially driving global climate change over several time scales. Direct and indirect …

The first results of the UVic Earth System Model coupled to a land surface scheme and a
dynamic global vegetation model are presented in this study. In the first part the present day …

Late Quaternary Environmental Change addresses the interaction between human agency
and other environmental factors in the landscapes, particularly of the temperate zone …

Using glacial rebound models we have inverted observations of crustal rebound and
shoreline locations to estimate the ice thickness for the major glaciations over northern …

This authoritative new text provides a thorough, updated account of glaciers and ice sheets
as monitors and indicators of environmental change. It examines the record of …

The North American Ice Sheet Complex played a major role in global sea level fluctuations
during the Late Quaternary but our knowledge of its dynamics is based mostly on its demise …

The US mid-Atlantic sea-level record is sensitive to the history of the Laurentide Ice Sheet as
the coastline lies along the ice sheet's peripheral bulge. However, paleo sea-level markers …