Opportunity Overview
Thinning is most prominent in the Amundsen Sea sector of the ice sheet, where it has been observed to spread inland from the coast, and to affect neighbouring outflow glaciers in a similar way. Those facts demonstrate that some change in ocean-driven melting of the glacier termini has been the trigger of change, leading to a widespread belief that warming of the ocean waters, driven ultimately by global warming, is responsible. However, observations of ocean temperature in the Amundsen Sea suggest a more complex history. The records start in 1994, and include only a few observations prior to 2009, but suggest cycles between warm and cool conditions occurring over decadal periods. That motivates a major rethink of how the ocean interacts with the ice sheet to produce the observed thinning.
In this project we plan to exploit new techniques to fill the gaps in the record of ocean temperature change in the Amundsen Sea. We will modify a robotic submarine so that it can over-winter beneath the pack ice, periodically measuring the properties and strength of the currents carrying warm water towards the ice. Those measurements will be complemented by fixed instruments that record continuously at selected locations and seal-borne sensors that will record the depth of the warm water wherever and whenever the seals dive below the surface to feed. We will relate these detailed observations of what is...
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Start FreeSolicitation Details
| Issuing agency | NERC |
|---|---|
| Country | United Kingdom |
| Category | Research Development |
| Published | June 30, 2020 |
| Procurement stage | Active solicitation |
| Response due | August 30, 2028 |
| Status | Open — accepting responses |
| Official source | View original notice |
| Last verified | August 09, 2026 |
Source: UK Research and Innovation (UKRI) — Open Government Licence v3.0.
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