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Ocean Interaction with Antarctic Ice Shelves

Objective

The primary goal OceanIS is to constrain the contribution of changes in Southern Ocean circulation to the recent acceleration in Antarctic Ice Sheet mass loss. Improving our knowledge of ice shelf–ocean interactions is a critical step toward reducing uncertainty in future sea level rise projections. Ice shelves are coastal areas of floating ice that extend from an ice sheet out over the ocean, and their destabilization can trigger rapid ice discharge. It is now evident that ocean–driven basal melt is the major cause of ice loss from Antarctica’s fringing ice shelves. However much of the fundamental dynamics of how the ocean delivers heat to the ice shelves remains unresolved. Progress in this area requires bringing together the fields of ice shelf–ocean interactions and large–scale Southern Ocean oceanography. The Southern Ocean overturning entails the upwelling of Circumpolar Deep Water (CDW) offshore Antarctica. The Antarctic Circumpolar Current has shifted poleward, the impact of which, e.g. over the upwelling of CDW, remains unknown. Since CDW is linked to the highest ice shelf thinning rates yet observed, the variability of the CDW properties and its interaction with the ice shelves is the focus of this proposal. To do this, OceanIS integrates, for the first time, several unique data sets, which extend from the deep ocean to the sub–ice shelf environment. These include data from the Argo network, instrumented seals, and measurements from the only decadal–scale record of ocean properties beneath an Antarctic ice shelf, the Amery ice shelf. OceanIS will help to test which of the suite of current climate models shows ice–ocean interaction processes and CDW variability that are most in line with reality. Given that the forcings driving Southern Ocean changes are expected to continue in the future, results of OceanIS will be a major step toward reducing the uncertainty that surrounds the future stability of the Antarctic Ice Sheet and sea level rise projections.

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Keywords

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Programme(s)

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Topic(s)

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Funding Scheme

Funding scheme (or “Type of Action”) inside a programme with common features. It specifies: the scope of what is funded; the reimbursement rate; specific evaluation criteria to qualify for funding; and the use of simplified forms of costs like lump sums.

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

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Call for proposal

Procedure for inviting applicants to submit project proposals, with the aim of receiving EU funding.

(opens in new window) H2020-MSCA-IF-2014

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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.

€ 195 454,80
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.

€ 195 454,80
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