Hydroclimatic changes associated with global warming over the past 50 years have been
documented widely, but physical landscape responses are poorly understood thus far …

Higher boreal summer insolation in the early to middle Holocene drove thousands of years
of summer warming across the Arctic. Modern-day warming has distinctly different causes …

Abstract In the Northern Hemisphere, an insolation driven Early to Middle Holocene Thermal
Maximum was followed by a Neoglacial cooling that culminated during the Little Ice Age …

We review paleoceanographic and paleoclimatic records from the northern North Atlantic to
assess the nature of climatic conditions at 4.2 ka BP, which has been identified as a time of …

Assessments of present and future flood hazard are often limited by the scarcity and short
time span of the instrumental time series. In pursuit of documenting the occurrence and …

This study proposes an integrated methodology which includes pedological, petrographic,
mineralogical and geochemical analyses of transparent heavy-minerals, to reconstruct the …

Carbon sequestration by sediments and vegetated marine systems contributes to
atmospheric carbon drawdown, but little empirical evidence is available to help separate the …

Local glaciers and ice caps (GICs) respond sensitively and quickly, on the scale of decades
to centuries, to climate variations. Continuous records of past fluctuations in GIC size provide …

A process-based understanding of lacustrine deposited sediments in Arctic lakes is
essential to set the present warming and hydroclimatic shift into perspective. From such a …

Glaciers and ice caps (GICs) respond rapidly to changes in temperature and precipitation.
Thus, records of their past fluctuations yield valuable information on past climate. However …