Offshore freshening of groundwater has been observed over 100 km off Norway’s coast, sometimes beyond the continental shelf. Yet, no previous studies have modeled freshened groundwater emplacement along the Norwegian continental margin. This study employs a hydrogeological model to simulate groundwater flow along a two-dimensional transect driven by mechanical loading during the Late Pleistocene and Holocene, encompassing thre...

The glacial isostatic adjustment (GIA) of the British Isles is complex due to the interplay between local and non‐local signals. A number of recent studies have modelled the GIA response of the British Isles using relative sea‐level data. This study extends these previous analyses by using output from a numerical glaciological model as input to a GIA model. This is a necessary step towards more realistic GIA models, and althou...