Ocean tide influences on the Antarctic and Greenland ice sheets
Ocean tides are the main source of high‐frequency variability in the vertical and horizontal
motion of ice sheets near their marine margins. Floating ice shelves, which occupy about …
motion of ice sheets near their marine margins. Floating ice shelves, which occupy about …
The dynamics of Greenland's glacial fjords and their role in climate
Rapid mass loss from the Greenland Ice Sheet has sparked interest in its glacial fjords for
two main reasons: Increased submarine melting of glaciers terminating in fjords is a …
two main reasons: Increased submarine melting of glaciers terminating in fjords is a …
[HTML][HTML] How does glacier discharge affect marine biogeochemistry and primary production in the Arctic?
Freshwater discharge from glaciers is increasing across the Arctic in response to
anthropogenic climate change, which raises questions about the potential downstream …
anthropogenic climate change, which raises questions about the potential downstream …
Future evolution of Greenland's marine‐terminating outlet glaciers
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 …
response to changes in global climate, motivating the scientific community to question how …
Bathymetry constrains ocean heat supply to Greenland's largest glacier tongue
J Schaffer, T Kanzow, WJ von Appen… - Nature …, 2020 - nature.com
Mass loss from the Greenland ice sheet has increased over the past two decades, currently
accounting for 25% of global sea-level rise. This is due to increased surface melt driven by …
accounting for 25% of global sea-level rise. This is due to increased surface melt driven by …
Where glaciers meet water: Subaqueous melt and its relevance to glaciers in various settings
Glacier change is ubiquitous, but the fastest and largest magnitude changes occur in
glaciers that terminate in water. This includes the most rapidly retreating glaciers, and also …
glaciers that terminate in water. This includes the most rapidly retreating glaciers, and also …
Twenty-first century ocean forcing of the Greenland ice sheet for modelling of sea level contribution
Abstract Changes in ocean temperature and salinity are expected to be an important
determinant of the Greenland ice sheet's future sea level contribution. Yet, simulating the …
determinant of the Greenland ice sheet's future sea level contribution. Yet, simulating the …
Nutrient release to oceans from buoyancy-driven upwelling at Greenland tidewater glaciers
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 …
potentially important contributor to regional marine primary production and nutrient cycling …
[HTML][HTML] A simple shelf circulation model: intrusion of Atlantic Water on the West Spitsbergen Shelf
F Nilsen, R Skogseth… - Journal of Physical …, 2016 - journals.ametsoc.org
Christoffersen, P., RI Mugford, KJ Heywood, I. Joughin, JA Dowdeswell, JPM Syvitski, A.
Luckman, and TJ Benham, 2011: Warming of waters in an East Greenland fjord prior to …
Luckman, and TJ Benham, 2011: Warming of waters in an East Greenland fjord prior to …
Modeling the impact of glacial runoff on fjord circulation and submarine melt rate using a new subgrid‐scale parameterization for glacial plumes
The injection at depth of ice sheet runoff into fjords may be an important control on the frontal
melt rate of tidewater glaciers. Here we develop a new parameterization for ice marginal …
melt rate of tidewater glaciers. Here we develop a new parameterization for ice marginal …