West Greenland has been intensively studied to reconstruct and better understand past
relative sea level changes and deglacial history. This study extends these efforts by linking …

The pattern of Greenland Ice Sheet margin change during the 20th century is variable. Large-
scale retreat of marine-outlet glaciers contrasts with the often-negligible retreat observed …

Microbial processes that mineralize organic carbon and enhance solute production at the
bed of polar ice sheets could be of a magnitude sufficient to affect global elemental cycles …

During the Last Glacial Period, the climate shift to cold conditions associated with changes
in atmospheric circulation and vegetation cover resulted in the development of large aeolian …

Glaciers and ice sheets cover over 10% of Earth's land surface area and store a globally
significant amount of dissolved organic matter (DOM), which is highly bioavailable when …

Jökulhlaups in 2007 and 2008 from an ice-dammed lake at the northern margin of Russell
Glacier, West Greenland, marked the onset of a renewed jökulhlaup cycle after 20 years of …

There has been a progressive increase in the number and area of ice-marginal lakes
situated along the south-western margin of the Greenland Ice Sheet (GrIS) since the 1980s …

Neoglacial and Little Ice Age (LIA) limits occur within 2km of the Inland Ice margin in the
Kangerlussuaq area on west Greenland. The LIA limit is clearly demarcated by ice‐cored …

Global change is reshaping the physical environment and altering nutrient dynamics across
the Arctic. These changes can affect the structure and function of biological communities and …

Meltwater discharge from the Greenland Ice Sheet (GrIS) exports sediment, solutes, total
phosphorus (TP), dissolved inorganic nitrogen (DIN), and other macro-and micronutrients to …