West Greenland Current
Top View
- Hydrographic Conditions Off West Greenland in 2016
- Ocean Circulation Causes the Largest Freshening Event for 120 Years in Eastern Subpolar North Atlantic
- Greenland Ice Mass Loss During the Younger Dryas Driven by Atlantic
- Holocene Climate Change in Arctic Canada and Greenland
- Mean Conditions and Seasonality of the West Greenland Boundary Current System Near Cape Farewell
- A High-Resolution Elemental Record of Post-Glacial
- Durham Research Online
- Scientific Council Report About Hydrographic Conditions Off West
- Holocene Paleoceanography of the Northeast Greenland Shelf
- The Water Masses and Currents of the Oceans Within Anygiven Region, the Character of the Water Massesdepends Mainly Upon Three F
- Evolution of the Freshwater Coastal Current at the Southern Tip of Greenland
- Hydrographic Conditions Off West Greenland in 2014
- Ocean Circulation Causes the Largest Freshening Event for 120 Years in Eastern Subpolar North Atlantic
- THE OCEAN CURRENTS by Prof A. Balasubramanian Objectives: After
- Meltwater Routing and the Younger Dryas
- Present Conditions in Greenland and the Kangerlussuaq Area
- Arctic Seas from Model Experiments with Passive Tracers
- Intensification of the Atlantic Deep Circulation by the Canadian Archipelago Throughflow