Ocean2Ice
Lead Research Organisation:
University of Southampton
Department Name: Sch of Ocean and Earth Science
Abstract
Detailed in the Lead Organization (University of East Anglia) proposal.
Planned Impact
Detailed in the Lead Organization (University of East Anglia) proposal.
Organisations
People |
ORCID iD |
Alberto Naveira Garabato (Principal Investigator) |
Publications
Brearley J
(2017)
Controls on turbulent mixing on the West Antarctic Peninsula shelf
in Deep Sea Research Part II: Topical Studies in Oceanography
Dotto T
(2018)
Variability of the Ross Gyre, Southern Ocean: Drivers and Responses Revealed by Satellite Altimetry
in Geophysical Research Letters
Garabato AC
(2017)
Vigorous lateral export of the meltwater outflow from beneath an Antarctic ice shelf.
in Nature
Heywood K
(2016)
Between the Devil and the Deep Blue Sea: The Role of the Amundsen Sea Continental Shelf in Exchanges Between Ocean and Ice Shelves
in Oceanography
Kimura S
(2016)
Ocean mixing beneath Pine Island Glacier ice shelf, West Antarctica OCEAN MIXING BENEATH PIG
in Journal of Geophysical Research: Oceans
Loose B
(2018)
Evidence of an active volcanic heat source beneath the Pine Island Glacier.
in Nature communications
Description | The research supported by this award has led to two key findings: - Oceanic mixing in the cavity beneath Pine Island Glacier (one of the fastest-melting glaciers in Antarctica) is enhanced above a submarine ridge, and promotes the transport of heat toward the base of the glacier. - The meltwater outflow from Pine Island Glacier is subject to a type of dynamical instability that prevents it from ascending to the ocean surface. An idealised model indicates that this instability is likely widespread around Antarctica, with important consequences for how accelerated Antarctic melting will influence the climate system. |
Exploitation Route | The above findings are likely to lead to significant advances in climate-scale models of ocean - ice sheet interactions. |
Sectors | Environment Other |
Description | In this award, we have resolved the long-standing question on why meltwater from the Antarctic Ice Sheet settles at depth instead of rising to the ocean surface. This will impact future climate-scale model development for climate and sea level rise projections. |
First Year Of Impact | 2017 |
Sector | Environment |