Freshwater thickness, pycnocline depth, and depth averaged velocities from 17 model scenarios in Admiralty Bay, Antarctica.

• Main Author: Osińska, Maria
• Format: Other/Unknown Material
• Language: unknown
• Published: Zenodo 2023
• Subjects: Antarc*; Antarctica
• Online Access: https://doi.org/10.5281/zenodo.10277333

The dataset contains model results from the Admiralty Bay hydrodynamic model calculated using the Delft3D Flow. It contains freshwater thickness (FWT), pycnocline depth, and depth-averaged velocities mean values from period 1.1.2022-28.01.2022, from 17 model scenarios. Scenarios details: 1–14 scenarios with increasing glacial influx (m^3/s per ~1 km of ice/water boundary) spread homogenously across glacial fronts with 0 m/s initial velocity: 1 - 0; 2 - 0.15 3 - 0.3; 4 - 0.6; 5 - 0.9; 6 -1.7; 7 - 3.0; 8 - 4.5; 9 - 6.0 (also described as test run H0); 10 - 8.0; 11 -11.0; 12 - 14.0; 13 - 28.0 14 - 60.0; 15 - H2 test run with glacial water discharged from all glaciers, homogenously through the entirety of glacial front, with an initial velocity of 2 m/s 16 - S0 test run with glacial water discharged from all glaciers subglacially, with zero initial velocity 17 - S2 test run with glacial water discharged from all glaciers subglacially, with an initial velocity of 2 m/s