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 The Greenland Ice Sheet (GIS) is losing mass at a high rate. Given the short-term
nature of the observational record, it is difficult to assess the historical importance of this …

Multibeam bathymetric and seismostratigraphic data collected in the Clyde fjord-cross-shelf
trough system (eastern Baffin Island, Canadian Arctic Archipelago) display glacial landforms …

Arctic precipitation is predicted to increase this century. Records of past precipitation
seasonality provide baselines for a mechanistic understanding of the dynamics controlling …

Surface mass loss from the Greenland ice sheet (GrIS) has accelerated over the past
decades, mainly due to enhanced surface melting and liquid water runoff in response to …

Changing climatic conditions is a perpetual circumstance for mankind. In this study, we
investigate local environmental and climatic changes near Kangerlussuaq, west Greenland …

The Greenland Ice Sheet is a key contributor to contemporary global sea level rise, but its
long-term history and response to episodes of warming in Earth's geological past remain …

An accurate record of preindustrial (pre-1900 CE) sea level is necessary to contextualize
modern global mean sea level (GMSL) rise with respect to natural variability. Precisely dated …

Stable isotopes of oxygen (δ 18 O) and hydrogen (δ 2 H) in precipitation are widely
employed tracers of the global hydrologic cycle, and are frequently inferred from lake-water …

Sometime during the middle to late Holocene (8.2 ka to∼ 1850–1900 CE), the Greenland
Ice Sheet (GrIS) was smaller than its current configuration. Determining the exact …