Previous rapid thinning of Pine Island Glacier sheds light on future Antarctic ice loss
(21 February 2014)
Researchers from the UK, USA and Germany found that Pine Island Glacier (PIG), which is rapidly accelerating, thinning and retreating, has thinned rapidly before. The team say their findings, published in the journal Science, demonstrate the potential for current ice loss to continue for several decades yet.
Their findings reveal that 8,000 years ago the glacier thinned as fast as it has in recent decades, providing an important model for its future behaviour. The glacier is currently experiencing significant acceleration, thinning and retreat that is thought to be caused by ‘ocean-driven’ melting - an increase in warm ocean water finding its way under the ice shelf.
After two decades of rapid ice loss, concerns are arising over how much more ice will be lost to the ocean in the future.
Model projections of the future of PIG contain large uncertainties, leaving questions about the rate, timing and persistence of future sea level rise.
Rocks exposed by retreating or thinning glaciers provide evidence of past ice sheet change, which helps scientists to predict possible future change. The geologists used highly sensitive dating techniques to track the thinning of PIG through time, and to show that the past thinning lasted for several decades.
Professor Mike Bentley, a co-leader of the project based in the Department of Geography, at Durham University, said: “This paper is part of a wide range of international scientific efforts to understand the behaviour of this important glacier.
“The results we’re publishing are the product of long days spent sampling rocks from mountains in Antarctica, coupled to some exceptionally precise and time-consuming laboratory analyses.
“The results are clear in showing a remarkably abrupt thinning of the glacier 8,000 years ago.”
Lead author Dr Joanne Johnson, from the British Antarctic Survey (BAS), said: "Our geological data show us the history of Pine Island Glacier in greater detail than ever before.
“The fact that it thinned so rapidly in the past demonstrates how sensitive it is to environmental change; small changes can produce dramatic and long-lasting results.
“Based on what we know, we can expect the rapid ice loss to continue for a long time yet, especially if ocean-driven melting of the ice shelf in front of Pine Island Glacier continues at current rates."
The research was funded by the Natural Environment Research Council and Lamont-Doherty Earth Observatory, USA (through a Marie Tharp fellowship awarded to Joanne Johnson). Logistical support was provided by the Alfred Wegener Institute