2024 Articles
High Salinity Shelf Water production rates in Terra Nova Bay, Ross Sea from high-resolution salinity observations
High Salinity Shelf Water (HSSW) formed in the Ross Sea is a precursor to Antarctic Bottom Water (AABW), a water mass that constitutes the bottom limb of the global overturning circulation. HSSW production rates are poorly constrained, as in-situ observations are scarce. Here, we present high-vertical-and-temporal-resolution salinity time series collected in austral winter 2017 from a mooring in Terra Nova Bay (TNB), one of two major sites of HSSW production in the Ross Sea. We calculate an annual-average HSSW production rate of ~0.4 Sv (10^6 m^3 s^(-1)), which we use to ground truth additional estimates across 2012 - 2021 made from parametrized net surface heat fluxes. We find sub-seasonal and interannual variability on the order of 0.1 Sv, with a strong dependence on variability in open-water area that suggests a sensitivity of TNB HSSW production rates to changes in the local wind regime and offshore sea ice pack.
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Files
- Miller_2024_Nature_Comms.pdf application/pdf 3.12 MB Download File
Also Published In
- Title
- Nature Communications
- DOI
- https://doi.org/10.1038/s41467-023-43880-1
More About This Work
- Academic Units
- Earth and Environmental Sciences
- Lamont-Doherty Earth Observatory
- Ocean and Climate Physics
- Published Here
- March 5, 2024