Oceanic heat flux towards Greenland’s tidewater glaciers depends on the rate of fjord-shelf exchange, the properties of the ocean waters entering the fjords, and how those waters are modified during fjord transit prior to interacting with tidewater glaciers15. Off the coast of Greenland, two wa...
which is essential in the context of climate change.#Dynamic glacier fracture and the subsequent generation and propagation of iceberg-induced tsunamis are reproduced using a unified numerical glacier–ocean model, in line with observations at the Eqip Sermia glacier in Greenland, as well as labora...
The Norwegian Atlantic Current in the Lofoten basin inferred from hydrological and tracer data (129I) and its interaction with the Norwegian Coastal Current Geophys. Res. Lett., 31 (1) (2004) Google Scholar Gebhardt et al., 2011 A.C. Gebhardt, W. Jokat, F. Niessen, J. Matthießen...
Figure 9. Wave interaction with iceberg in experiments 2 (a) and 3 (b). The iceberg masses and heights measured in experiments 1–8 are given in Table 3 and in Figure 10 versus the time. In all experiments, the masses and heights of the icebergs decreased, and their dependencies on ...
Rignot, E.; Fenty, I.; Xu, Y.; Cai, C.; Velicogna, I.; Cofaigh, C.O.; Dowdeswell, J.A.; Weinrebe, W.; Catania, G.; Duncan, D. Bathymetry data reveal glaciers vulnerable to ice-ocean interaction in Uummannaq and Vaigat glacial fjords, west Greenland.Geophys. Res. Lett.2016...