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Office of Polar Programs


Thwaites: The Future of Thwaites Glacier and its Contribution to Sea-level Rise


CONTACTS
Name Email Phone Room
Paul  . Cutler pcutler@nsf.gov (703) 292-4961   


PROGRAM GUIDELINES

Solicitation  17-505

Important Information for Proposers

ATTENTION: Proposers using the Collaborators and Other Affiliations template for more than 10 senior project personnel will encounter proposal print preview issues. Please see the Collaborators and Other Affiliations Information website for updated guidance.

A revised version of the NSF Proposal & Award Policies & Procedures Guide (PAPPG) (NSF 18-1), is effective for proposals submitted, or due, on or after January 29, 2018. Please be advised that, depending on the specified due date, the guidelines contained in NSF 18-1 may apply to proposals submitted in response to this funding opportunity.


SYNOPSIS

Considerable uncertainty remains in projections of future ice loss from West Antarctica.  Reducing this uncertainty is an international priority that was recently underscored by the Scientific Committee on Antarctic Research in its “Horizon Scan 2020” (SCAR, 2015). The recent U.S. National Academy of Sciences, Engineering, and Medicine report (A Strategic Vision for NSF Investments in Antarctic and Southern Ocean Research, 2015) places prediction of ice mass loss from the West Antarctic Ice Sheet (WAIS) as the top priority for Antarctic research, and singles out Thwaites Glacier as a “region of particular concern”.

Building on this community priority, and recognizing that such research is becoming an increasingly global endeavor with demands that exceed the capacities of any one nation, NSF and the UK Natural Environment Research Council (NERC) have developed this joint program with the objective to substantially improve both decadal and longer-term (century-to-multi-century) projections of ice loss and sea-level rise originating from Thwaites Glacier.

Since the 1990s, satellites have shown accelerating ice loss driven by ocean change in five neighboring glacier catchments, including Thwaites Glacier, that drain more than one third of the WAIS. The rate of ice loss there doubled in six years and now accounts for about 10 percent of global sea-level rise. The most rapid ice loss is currently from Pine Island Glacier, which has been the focus of the NERC iSTAR Programme and NSF-funded science.  Recent studies indicate the greatest risk for future rapid sea-level rise now arises from Thwaites Glacier due to the large changes already underway, the potential contribution to sea-level rise, and the societally relevant timescales of decades to centuries over which major, irreversible changes are possible in the system.

The program will have a direct and significant impact on understanding the stability of marine ice sheets and specifically the West Antarctic Ice Sheet in the vicinity of Thwaites Glacier, and will contribute to the ice-sheet modeling community capability to simulate ice sheets and to reduce the uncertainties in sea-level projections. In addition, the program will contribute to improving risk assessments that coastal communities need for decisions about adaptation and long-range planning.

What Has Been Funded (Recent Awards Made Through This Program, with Abstracts)

Map of Recent Awards Made Through This Program