Evolution of climate anomalies and variability of Southern Ocean water masses on interannual to centennial time scales

• Main Author: Santoso, Agus
• Format: Doctoral or Postdoctoral Thesis
• Language: English
• Published: UNSW, Sydney 2005
• Subjects: Climatic changes > Mathematical models; Ocean-atmosphere interaction > Mathematical models; Antarctic; Indian; Southern Ocean; Weddell; Weddell Sea; Antarc*; North Atlantic Deep Water; North Atlantic
• Online Access: http://hdl.handle.net/1959.4/33355; https://unsworks.unsw.edu.au/bitstreams/a53ff4ce-9958-4be1-b724-d6db088a116e/download; https://doi.org/10.26190/unsworks/17768

In this study the natural variability of Southern Ocean water masses on interannual to centennial time scales is investigated using a long-term integration of the Commonwealth Scientic and Industrial Research Organisation (CSIRO) coupled climate model. We focus our attention on analysing the variability of Antarctic IntermediateWater (AAIW), Circumpolar DeepWater (CDW), and Antarctic Bottom Water (AABW). We present an analysis of the dominant modes of temperature and salinity (T - S) variability within these water masses. Climate signals are detected and analysed as they get transmitted into the interior from the water mass formation regions. Eastward propagating wavenumber-1, -2, and -3 signals are identied using a complex empirical orthogonal function (CEOF) analysis along the core of the AAIW layer. Variability in air-sea heat uxes and ice meltwater rates are shown by heat and salt budget analyses to control variability of Antarctic Surface Water where density surfaces associated with AAIW outcrop. The dominant mode in the CDW layer is found to exhibit an interbasin-scale of variability originating from the North Atlantic, and propagating southward into the Southern Ocean. Salinity dipole anomalies appear to propagate around the Atlantic meridional overturning circulation with the strengthening and weakening of North Atlantic Deep Water formation. In the AABW layer, T - S anomalies are shown to originate from the southwestern Weddell Sea, driven by salinity variations and convective overturning in the region. It is also demonstrated that the model exhibits spatial patterns of T - S variability for the most part consistent with limited observational record in the Southern Hemisphere. However, some observations of decadal T - S changes are found to be beyond that seen in the model in its unperturbed state. We further assess sea surface temperature (SST) variability modes in the Indian Ocean on interannual time scales in the CSIRO model and in reanalysis data. The emergence of a meridional SST dipole during ...