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Southern Ocean Overtuning Fingerprint Experiment

Project description

Quantifying the hydrographic fingerprint of the overturning water circulation

As a continuous ring of water around Antarctica, the Southern Ocean links all other oceans. The process of overturning circulation influences powerfully Earth’s climate. While numerical studies suggest there are substantial variations in the overturning circulation due to increased westerly winds, there is a lack of observational evidence that these variations have occurred or are occurring in oceanographic measurements. The EU-funded SOFIE project aims to detect and measure the hydrographic fingerprint of changes in this overturning. SOFIE proposes that changes in the overturning circulation affect noticeably the ocean interior density structure from surface to depth across the Southern Ocean. It will test this hypothesis in the state-of-the-art numerical NEMO-OPA model.

Objective

The Southern Ocean overturning circulation exerts a powerful influence on Earth’s climate, and SOFIE is the first project seeking to detect and objectively measure the hydrographic fingerprint of changes in this overturning.The deep waters upwelling in the Southern Ocean account for up to half of the annual oceanic uptake of anthropogenic carbon from the atmosphere, dominate the global oceanic heat uptake with up to three quarters of the additional heat influx to the ocean occurring south of 30°S, and are a rich source of the nutrients that fertilise the majority of global ocean biological productivity north of 30°S.According to numerical studies, there is consensus that in response to increased westerly winds such as those occurring within contemporary climate change, variations in the overturning circulation are likely to be substantial.However there is no established approach to provide observational evidence that these variations have occurred or are occurring in oceanographic measurements;and the lack of such an approach stems from the uncertain fingerprint of Southern Ocean overturning circulation changes on measurable oceanographic variables.Based on preliminary results supported by recent studies, SOFIE proposes that changes in the overturning circulation affect discernibly the ocean interior density structure from surface to depth across the Southern Ocean.We will rigorously test this hypothesis in the state-of-the-art numerical NEMO-OPA model, and assess in-situ evidence of overturning changes from the pan–Antarctic Argo network.To do this, SOFIE will combine model diagnostics of the Southern Ocean overturning circulation with the application to the model and in-situ fields of a novel algorithm characterising the vertical structure of the ocean.Given the ocean overturning’s sensitivity to changes in atmospheric forcing,SOFIE results will be a major step to constrain the changing ability of the Southern Ocean to slow down the rate of global climate change.

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MSCA-IF - Marie Skłodowska-Curie Individual Fellowships (IF)

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Call for proposal

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(opens in new window) H2020-MSCA-IF-2018

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Coordinator

UNIVERSITY OF SOUTHAMPTON
Net EU contribution

Net EU financial contribution. The sum of money that the participant receives, deducted by the EU contribution to its linked third party. It considers the distribution of the EU financial contribution between direct beneficiaries of the project and other types of participants, like third-party participants.

€ 224 933,76
Address
Highfield
SO17 1BJ SOUTHAMPTON
United Kingdom

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Region
South East (England) Hampshire and Isle of Wight Southampton
Activity type
Higher or Secondary Education Establishments
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Total cost

The total costs incurred by this organisation to participate in the project, including direct and indirect costs. This amount is a subset of the overall project budget.

€ 224 933,76
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