Articles | Volume 19, issue 2
https://doi.org/10.5194/os-19-381-2023
https://doi.org/10.5194/os-19-381-2023
Research article
 | 
04 Apr 2023
Research article |  | 04 Apr 2023

Water mass transformation variability in the Weddell Sea in ocean reanalyses

Shanice T. Bailey, C. Spencer Jones, Ryan P. Abernathey, Arnold L. Gordon, and Xiaojun Yuan

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Cited articles

Abernathey, R. P., Cerovecki, I., Holland, P. R., Newsom, E., Mazloff, M., and Talley, L. D.: Water-mass transformation by sea ice in the upper branch of the Southern Ocean overturning, Nat. Geosci., 9, 596–601, https://doi.org/10.1038/ngeo2749, 2016. a, b, c
Armitage, T. W. K., Kwok, R., Thompson, A. F., and Cunningham, G.: Dynamic Topography and Sea Level Anomalies of the Southern Ocean: Variability and Teleconnections, J. Geophys. Res.-Oceans, 123, 613–630, https://doi.org/10.1002/2017JC013534, 2018. a
Bailey, S.: Water mass transformation variability in the Weddell Sea in Ocean Reanalyses, Zenodo [code], https://doi.org/10.5281/zenodo.7776037, 2023. a
Brown, P. J., Jullion, L., Landschützer, P., Bakker, D. C. E., Naveira Garabato, A. C., Meredith, M. P., Torres-Valdés, S., Watson, A. J., Hoppema, M., Loose, B., Jones, E. M., Telszewski, M., Jones, S. D., and Wanninkhof, R.: Carbon dynamics of the Weddell Gyre, Southern Ocean, Global Biogeochem. Cy., 29, 288–306, https://doi.org/10.1002/2014GB005006, 2015. a
Buckley, M., Campin, J.-M., Chaudhuri, A., Fenty, I., Forget, G., Fukumori, I., Heimbach, P., Hill, C., King, C., Liang, X., Nguyen, A., Piecuch, C., Ponte1, R., Quinn, K., Sonnewald, M., Spiege, D., Vinogradova, N., Wang, O., and Wunsch, C.: The ECCO Consortium: A Twenty-Year Dynamical Oceanic Climatology: 1994–2013. Part 2: Velocities, Property Transports, Meteorological Variables, Mixing Coefficients, MIT Libraries [preprint], http://hdl.handle.net/1721.1/109847 (last access: 1 March 2023), 2017. a
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Short summary
This study explores the variability of water mass transformation within the Weddell Gyre (WG). The WG is the largest source of Antarctic Bottom Water (AABW). Changes to our climate can modify the mechanisms that transform waters to become AABW. In this study, we computed water mass transformation volume budgets by using three ocean models and a mathematical framework developed by Walin. Out of the three models, we found one to be most useful in studying the interannual variability of AABW.