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 …

Abstract Purpose of Review Assessment of the impact of ocean resolution in Earth System
models on the mean state, variability, and future projections and discussion of prospects for …

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

Feedbacks between ice melt, glacier flow and ocean circulation can rapidly accelerate ice
loss at tidewater glaciers and alter projections of sea-level rise. At the core of these …

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 …

Mass loss from the Greenland ice sheet (GrIS) has increased over the last two decades in
response to changes in global climate, motivating the scientific community to question how …

Greenland runoff, from ice mass loss and increasing rainfall, is increasing. That runoff, as
discharge, impacts the physical, chemical, and biological properties of the adjacent fjords …

Submarine melting has been implicated as a driver of glacier retreat and sea level rise, but
to date melting has been difficult to observe and quantify. As a result, melt rates have been …

Submarine melting of Greenlandic tidewater glacier termini is proposed as a possible
mechanism driving their recent thinning and retreat. We use a general circulation model …

Abstract Meltwater from the Greenland Ice Sheet often drains subglacially into fjords, driving
upwelling plumes at glacier termini. Ocean models and observations of submarine termini …