Publications by authors named "Kjersti Daae"
Article Synopsis
- The movement of heat from the ocean to the Antarctic continental margin is crucial for understanding the Antarctic Ice Sheet's overall stability.
- Recent models indicate that the most significant heat transfer occurs where heavy shelf waters flow down the continental slope.
- Our observations using moored instruments support this by showing a connection between the downward flow of dense water and the upward flow of warmer water on the shelf.
