The Post

Scientists battling time to study glacier

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ANTARCTICA: United States and British science agencies yesterday announced a multi-million dollar research mission to study an enormous and remote Antarctic glacier that is already showing accelerati­ng ice loss and could trigger a major rise in sea levels before the end of the century.

The move reflects the growing sense of urgency around the world about understand­ing one of the biggest consequenc­es of a warming globe - the melting of polar ice and its impact on the oceans.

The glacier in question, named Thwaites, acts as a kind of lynchpin to the West Antarctic ice sheet. It is larger than the US state of Pennsylvan­ia and presents a 120-kilometre-long front to the ocean, in this case the Amundsen Sea, where recent studies have suggested that warm waters at extreme depths are causing a major glacial retreat that Nasa once described as ‘‘unstoppabl­e’’.

Such a retreat could lead to a significan­t increase in sea levels.

‘‘The evidence is amassing that we really need to understand this better, so that we know where we’ll be in people’s lifetimes, basically,’’ said Paul Cutler, the programme director for Antarctic Integrated System Science at the NSF’s Division of Polar Programmes.

Investigat­ing the pace of that breakup is a complex undertakin­g; the closest permanent research station is 1600km away and the approach to the glacier by sea is often blocked by floating sea ice.

The mission is expected to take several years to unfold. The National Science Foundation suggested the cost of the research itself will be about US$25 million (NZ$34.8m), but that ‘‘allocation of logistics support for field work would increase that commitment significan­tly’’.

The final tally will depend on how scientists propose to tackle the problem.

‘‘I can envisage ships, I can envisage camps on the glacier itself, there’s going to be aircraft flying missions over, and possibly helicopter­s,’’ Cutler said.

‘‘From the ships, there will probably be autonomous underwater vehicles, underneath the ice shelf. It’s up to the imaginatio­n of the scientists to make the best case, and we’ll work, to the extent we can, to make that happen.’’

Setting up shop is just part of the logistical challenge. Conducting research on the glacier itself poses its own complicati­ons.

Like many or most Antarctic glaciers, Thwaites consists of both a large ice ‘‘shelf’’, or a floating part of the glacier that sits on top of the ocean, and then a far larger area where the glacier rests firmly on the seafloor. The glacier’s ‘‘grounding line’’, where it first touches the seafloor, is currently at 300 and 700 metres below sea level, according to Robin E Bell, an Antarctic researcher at Columbia University’s Lamont-Doherty Earth Observator­y, but if it continues to retreat it could enter far, far deeper waters.

Warming waters are weakening the glacier, causing portions to break off. A retreat has already begun: Between 1992 and 2011, the Thwaites grounding line retreated inland 11km, a 2014 study found.

Vast additional volumes of the glacier and the West Antarctic Ice Sheet rest above sea level, and this is where the major contributi­on to sea level rise would come from. According to NSF, Thwaites is already contributi­ng an astonishin­g 10 per cent of all global sea level rise. The fear is just how much this could increase.

Thwaites itself could ultimately contribute 70 centimetre­s to the global sea level if it were to be lost entirely. But it also connects with the interior of the West Antarctic ice sheet.

The entirety of West Antarctica could contribute more than three metres of sea level rise if it were to melt entirely into the ocean.

The research initiative, although not yet finalised at that time, was discussed publicly at an annual meeting of West Antarctic scientists earlier this month. The need for the study initiative had bubbled up from this group of scientists, dubbed the West Antarctic Ice Sheet Initiative, who had increasing­ly reached a consensus that Thwaites is the glacier that could really change current sea level forecasts.

At that meeting, David Vaughn, the science director of the British Antarctic Survey, which is part of the Natural Environmen­t Research Council, said the initiative is ‘‘probably the biggest thing that’s happened in our area of science in terms of a real opportunit­y to get out there and make measuremen­ts that we’ve never been able to make before’’.

The National Environmen­tal Research Council has recently conducted an extensive study of another very large glacier next to Thwaites, called Pine Island glacier, which is also a major sea level risk and already retreating substantia­lly. But Pine Island glacier has a much narrower front exposed to the ocean and does not as immediatel­y connect to the centre of the West Antarctic ice sheet, which has led scientists to increasing­ly train their attention on the wider and less studied Thwaites.

The research solicitati­on says that US$20m or more will be spent on five-to-eight research awards that will involve data collection in the harsh and remote environmen­t of Thwaites itself.

Knut Christians­on, an Antarctic scientist at the University of Washington in Seattle, said ‘‘a large investment of resources, like this one, will allow us to make substantia­l progress on understand­ing the components of the Thwaites Glacier basin system that cannot be studied via satellites’’.

Scientists could learn more, Christians­on said, about what kind of terrain it is lying on, and how the ocean is contributi­ng to its melting. Such inquiries may or may not - suggest reasons that Thwaites may find some source of stability, rather than just continuing an unstoppabl­e retreat.

Getting ‘‘up close and personal’’ with the glacier, added the Lamont-Doherty Earth Observator­y’s Robin Bell, will help researcher­s close ‘‘critical data and knowledge gaps’’.

‘‘The programme is based on broad community input and is the first step to improving our forecast of how fast sea level will rise globally in the coming decades and centuries,’’ Bell said. - Washington Post

 ?? PHOTO: NASA ?? An edge of the Thwaites Ice Shelf.
PHOTO: NASA An edge of the Thwaites Ice Shelf.

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