In recent decades, the land-ocean aquatic continuum, commonly defined as the interface, or
transition zone, between terrestrial ecosystems and the open ocean, has undergone …

Glaciers cover about 10% of the Earth's land area but they are retreating rapidly and many
will disappear within decades. Glacier retreat is a worldwide phenomenon increasing the …

Accelerated mass loss from the Greenland ice sheet leads to glacier retreat and an
increasing input of glacial meltwater to the fjords and coastal waters around Greenland …

Freshwater discharge from glaciers is increasing across the Arctic in response to
anthropogenic climate change, which raises questions about the potential downstream …

The current downturn of the arctic cryosphere, such as the strong loss of sea ice, melting of
ice sheets and glaciers, and permafrost thaw, affects the marine and terrestrial carbon cycles …

Abstract Runoff from the Greenland Ice Sheet (GrIS) is thought to enhance marine
productivity by adding bioessential iron and silicic acid to coastal waters. However …

Recent archaeological and paleoecological work along both interior and coastal routes for
early colonization of the New World has suggested that the interior route was impossible …

The Arctic marine system is large and heterogeneous, harsh and remote, and now changing
very rapidly, all of which contribute to our current inadequate understanding of its basic …

Climate-change driven increases in temperature and precipitation are leading to increased
discharge of freshwater and terrestrial material to Arctic coastal ecosystems. These inputs …

Primary production on the coast and in Greenland fjords sustains important local and
sustenance fisheries. However, unprecedented melting of the Greenland Ice Sheet (GrIS) is …