Icelandic riverine freshwater distribution, offshore export, and alongshelf connectivity

This study models Iceland's shelf and surrounding ocean waters to quantify shelf distributions, flushing times, offshore exports (beyond the 400-m isobath), and alongshelf transports of Iceland's riverine freshwater. Analysis of the 2019 period divides the shelf into four quadrants and follows river waters delivered to each quadrant with tracked freshwater tracers that decay over time in open-ocean waters. Tracked freshwater thicknesses are large in the southwest quadrant and near major rivers in other areas. Freshwater is present around the entire shelf, but is less prevalent in the southeast quadrant. Many river waters can reach halfway around Iceland before being exported offshore; diminishing amounts can almost entirely circumnavigate Iceland. Annual average freshwater flushing times have an approximately seasonal scale at around 3 and 4 months for eastern and western river waters, respectively. Annual average freshwater exports are larger from northern shelf quadrants than southern ones. Average alongshelf freshwater transports are downshelf. Alongshelf connectivity is strong between most quadrants and moderate between the eastern quadrants. Regressions show how export and downshelf transport increase during upwelling-favorable and downwelling-favorable winds, respectively. Results indicate the Icelandic Coastal Current has robust buoyancy signatures and connected currents in western Iceland, and has generally weaker buoyancy and less-pronounced connected flows on the eastern side. • Freshwater thickness is large in southwest Iceland, which has the most discharge. • Freshwater flushing times are seasonal (3–4 months). • Exports are larger from northern shelf, increase with upwelling-favorable winds. • Alongshelf connectivity is strong, larger for downwelling-favorable winds. • Icelandic Coastal Current is strongest on western shelf and extends around Iceland.