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Interdecadal water mass changes in the Southern Ocean between 30°E and 160°E
Citation
Aoki, S and Bindoff, NL and Church, JA, Interdecadal water mass changes in the Southern Ocean between 30°E and 160°E, Geophysical Research Letters, 32, (7) pp. L07607. ISSN 0094-8276 (2005) [Refereed Article]
Abstract
Interdecadal water mass changes in the Indian - Western Pacific sectors of the Southern Ocean were investigated using the Japanese Antarctic Research Expeditions and historical hydrographic observations from the 1950s to 1990s. Freshening and cooling occurred on the neutral density surfaces of 27.0 kg�m−3 equatorward of Sub-Antarctic Front. Results for the area south of the Polar Front show warm and saline anomalies and oxygen decreases on the surfaces around 27.9 kg�m−3, which correspond to the Upper Circumpolar Deep Water. These latter anomalies are most simply explained by the mixing of these shallow waters with warmer and fresher surface waters. Steric sea level has also increased with an average change of 1mm�yr−1 from the 1970s to 1990s. The changes are larger north of the Sub-Antarctic Front, implying a strengthening of the Antarctic Circumpolar Current. It appears that the observed changes are consistent with the results from coupled climate model results for a similar period.
Item Details
Item Type: | Refereed Article |
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Research Division: | Earth Sciences |
Research Group: | Oceanography |
Research Field: | Physical oceanography |
Objective Division: | Environmental Management |
Objective Group: | Marine systems and management |
Objective Field: | Measurement and assessment of marine water quality and condition |
UTAS Author: | Bindoff, NL (Professor Nathan Bindoff) |
UTAS Author: | Church, JA (Dr John Church) |
ID Code: | 34683 |
Year Published: | 2005 |
Web of Science® Times Cited: | 58 |
Deposited By: | IASOS |
Deposited On: | 2005-08-01 |
Last Modified: | 2011-07-18 |
Downloads: | 0 |
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