The notion that the Atlantic Meridional Overturning Circulation (AMOC) can have more than
one stable equilibrium emerged in the 1980s as a powerful hypothesis to explain rapid …

Arguably, the most conspicuous evidence for anthropogenic climate change lies in the Arctic
Ocean. For example, the summer-time Arctic sea ice extent has declined over the last 40 …

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 …

The Greenland ice sheet has experienced increasing mass loss since the 1990s,. The
enhanced freshwater flux due to both surface melt and outlet glacier discharge is assuming …

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 …

Each summer, large quantities of freshwater and associated dissolved and particulate
material are released from the Greenland Ice Sheet (GrIS) into local fjords where they …

The discharge of nutrient-rich meltwater from the Greenland Ice Sheet has emerged as a
potentially important contributor to regional marine primary production and nutrient cycling …

Abstract The Beaufort Gyre (BG), the largest Arctic Ocean freshwater reservoir, has
drastically increased its liquid freshwater content by 40% in the past two decades. If …

The cumulative Greenland freshwater flux anomaly has exceeded 5,000 km3 since the
1990s. The volume of this surplus freshwater is expected to cause substantial freshening in …

Liquid freshwater fluxes from the Greenland ice sheet affect ocean water properties and
circulation on local, regional and basin-wide scales, with associated biosphere effects. The …