This project is supported by the Natural Environment Research Council, UK
This project will assess the dynamics of the outflow of Antarctic Bottom Water (AABW, a water mass formed near Antarctica that integrates the deepest layers of the global ocean’s overturning circulation) at one of its key sites of export from the subpolar Southern Ocean: the Orkney Passage. The project focuses on this passage following recent evidence that it channels the single most voluminous outflow of AABW from the Antarctic subpolar seas, and that it may be centrally implicated in the climatic changes exhibited by AABW in the Atlantic Ocean. The project is exciting because the new way in which we propose to look at the Orkney Passage outflow promises to deliver significant advances in our conceptual understanding of abyssal ocean circulation and its sensitivity to climatic variations in forcing, against a backdrop of remarkably rapid and widespread changes in AABW properties observed to be ongoing over much of the global ocean.
During the last three decades, AABW has exhibited a striking warming and contraction in volume over much of the global ocean abyss, particularly in the Atlantic basin. The causes of these changes are unknown. Possible explanations in terms of a climate-scale perturbation to the properties of the AABW precursor water masses near the Antarctic margins have been tentatively put forward by a number of authors, yet endorsement of these ideas by time series of water mass characteristics near the AABW sources is at best equivocal. In the Atlantic sector, observations strongly suggest a tantalizing alternative (or complementary) explanation: that climatic variations in the basin-scale properties of AABW downstream of its source region are primarily controlled by wind-forced changes in export, via a mechanism involving the modulation of small-scale turbulent mixing in the Orkney Passage.
We propose to test this emerging hypothesis by (i) measuring the circulation, water mass transformations and their underpinning physical processes in the passage for the first time, and (ii) assessing the climatic significance of those processes with a cost-effective enhancement of the BAS-supported mooring array presently deployed at the site.
Early 2015 – Deployment of DynOPO moorings
Early 2017 – DynOPO process cruise and mooring recovery
2017 – 2020 – Analysis of DynOPO data set
All data will be submitted to the British Oceanographic Data Centre (BODC), who will make it available to the community via usual channels (including rapid delivery for e.g. Argo calibration, and delayed post-QC mode).
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