Ocean Sci. Discuss., 8, 2197-2235, 2011
www.ocean-sci-discuss.net/8/2197/2011/
doi:10.5194/osd-8-2197-2011
© Author(s) 2011. This work is distributed
under the Creative Commons Attribution 3.0 License.
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This discussion paper has been under review for the journal Ocean Science (OS). Please refer to the corresponding final paper in OS.
Influence of Ross Sea Bottom Water changes on the warming and freshening of the Antarctic Bottom Water in the Australian-Antarctic Basin
K. Shimada1, S. Aoki1, K. I. Ohshima1, and S. R. Rintoul2,3,4,5
1Institute of Low Temperature Science, Hokkaido University, Sapporo, Japan
2CSIRO Marine and Atmospheric Research, Hobart, Tasmania, Australia
3Centre for Australian Weather and Climate Research, Hobart, Tasmania, Australia
4Antarctic Climate and Ecosystems Cooperative Research Centre, Hobart, Tasmania, Australia
5CSIRO Wealth from Oceans National Research Flagship, Hobart, Tasmania, Australia

Abstract. The WOCE Hydrographic Program (WHP) and repeated hydrographic data were used to document overall property changes of the Antarctic Bottom Water (AABW) in the Australian-Antarctic Basin between the 1990s and 2000s. Strong cooling and freshening is observed on isopycnals for layers denser than γn = 28.30. Changes in average salinity and potential temperature below this isopycnal correspond to basin-wide warming of 1300 ± 200 TW and freshening of 24 ± 3 Gt yr−1. While freshening can be explained by freshening of major source waters, i.e., the High Salinity Shelf Water (HSSW) of the Ross Sea and the dense shelf water formed in the Adélie and George V Land (AGVL) region, extensive warming of the AABW cannot be explained by warming of the source waters. A possible cause of warming of the AABW is a decrease in supply of the Ross Sea Bottom Water (RSBW). Hydrographic profiles between the Drygalski Trough of the Western Ross Sea and 150° E were analyzed in the context of a simple advective-diffusive model to assess the causes of the observed changes. The RSBW has also warmed by a larger amount than its source water (the HSSW). The model suggests that the warming of the RSBW observed between the 1970s and 2000s can be explained by a 21 ± 23% reduction in transport of the RSBW and an enhancement of the vertical diffusion of heat as a result of a 30 ± 7% weakening of the abyssal stratification. Freshening of the HSSW reduced the salinity and density stratification between the bottom water layer and overlying ambient water. Hence, freshening of the HSSW both directly freshened and indirectly warmed the RSBW by enhancing the vertical mixing. A simple box model suggest that changes in property and volume transport (decrease of 6.7% is assumed between the year 1995 and 2005) of the RSBW can explain 51 ± 6% of the warming and 84 ± 10% of the freshening observed in the AABW. These facts demonstrate that changes in both property and volume transport of the RSBW have contributed to the warming and freshening of the AABW in the Australian-Antarctic Basin.

Citation: Shimada, K., Aoki, S., Ohshima, K. I., and Rintoul, S. R.: Influence of Ross Sea Bottom Water changes on the warming and freshening of the Antarctic Bottom Water in the Australian-Antarctic Basin, Ocean Sci. Discuss., 8, 2197-2235, doi:10.5194/osd-8-2197-2011, 2011.
 
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