By Guest Author 13/07/2017

Adrian Luckman, Swansea University

One of the largest icebergs ever recorded has just broken away from the Larsen C Ice Shelf in Antarctica. Over the past few years I’ve led a team that has been studying this ice shelf and monitoring change. We spent many weeks camped on the ice investigating melt ponds and their impact – and struggling to avoid sunburn thanks to the thin ozone layer. Our main approach, however, is to use satellites to keep an eye on things.

We’ve been surprised by the level of interest in what may simply be a rare but natural occurrence. Because, despite the media and public fascination, the Larsen C rift and iceberg “calving” is not a warning of imminent sea level rise, and any link to climate change is far from straightforward. This event is, however, a spectacular episode in the recent history of Antarctica’s ice shelves, involving forces beyond the human scale, in a place where few of us have been, and one which will fundamentally change the geography of this region.

The iceberg would barely fit inside Wales. Adrian Luckman / MIDAS, Author provided
The ice shelves of the Antarctic peninsula. Note Larsen A and B have largely disappeared. AJ Cook & DG Vaughan, 2014, CC BY-SA

Ice shelves are found where glaciers meet the ocean and the climate is cold enough to sustain the ice as it goes afloat. Located mostly around Antarctica, these floating platforms of ice a few hundred meters thick form natural barriers which slow the flow of glaciers into the ocean and thereby regulate sea level rise. In a warming world, ice shelves are of particular scientific interest because they are susceptible both to atmospheric warming from above and ocean warming from below.

For the following century, the shelf, or what we now know to be a set of distinct shelves – Larsen A, B, C and D – remained fairly stable. However the sudden disintegrations of Larsen A and B in 1995 and 2002 respectively, and the ongoing speed-up of glaciers which fed them, focused scientific interest on their much larger neighbour, Larsen C, the fourth biggest ice shelf in Antarctica.Back in the 1890s, a Norwegian explorer named Carl Anton Larsen sailed south down the Antarctic Peninsula, a 1,000km long branch of the continent that points towards South America. Along the east coast he discovered the huge ice shelf which took his name.

The author prepares to assist his colleague, Bryn Hubbard from Aberystwyth University, in drilling a borehole in Larsen C using pressurised hot water. MIDAS, Author provided

This is why colleagues and I set out in 2014 to study the role of surface melt on the stability of this ice shelf. Not long into the project, the discovery by our colleague, Daniela Jansen, of a rift growing rapidly through Larsen C, immediately gave us something equally significant to investigate.

Nature at work

The development of rifts and the calving of icebergs is part of the natural cycle of an ice shelf. What makes this iceberg unusual is its size – at around 5,800 km² it’s the size of a small US state. There is also the concern that what remains of Larsen C will be susceptible to the same fate as Larsen B, and collapse almost entirely

Larsen B once extended hundreds of kilometres over the ocean. Today, one of its glaciers runs straight into the sea. Armin Rose / shutterstock

Our work has highlighted significant similarities between the previous behaviour of Larsen B and current developments at Larsen C, and we have shown that stability may be compromised. Others, however, are confident that Larsen C will remain stable.

What is not disputed by scientists is that it will take many years to know what will happen to the remainder of Larsen C as it begins to adapt to its new shape, and as the iceberg gradually drifts away and breaks up. There will certainly be no imminent collapse, and unquestionably no direct effect on sea level because the iceberg is already afloat and displacing its own weight in seawater.

This means that, despite much speculation, we would have to look years into the future for ice from Larsen C to contribute significantly to sea level rise. In 1995 Larsen B underwent a similar calving event. However, it took a further seven years of gradual erosion of the ice-front before the ice shelf became unstable enough to collapse, and glaciers held back by it were able to speed up, and even then the collapse process may have depended on the presence of surface melt ponds.


Even if the remaining part of Larsen C were to eventually collapse, many years into the future, the potential sea level rise is quite modest. Taking into account only the catchments of glaciers flowing into Larsen C, the total, even after decades, will probably be less than a centimetre.

Is this a climate change signal?

This event has also been widely but over-simplistically linked to climate change. This is not surprising because notable changes in the earth’s glaciers and ice sheets are normally associated with rising environmental temperatures. The collapses of Larsen A and B have previously been linked to regional warming, and the iceberg calving will leave Larsen C at its most retreated position in records going back over a hundred years.

However, in satellite images from the 1980s, the rift was already clearly a long-established feature, and there is no direct evidence to link its recent growth to either atmospheric warming, which is not felt deep enough within the ice shelf, or ocean warming, which is an unlikely source of change given that most of Larsen C has recently been thickening. It is probably too early to blame this event directly on human-generated climate change.

The ConversationYou may be interested in: When an Antarctic iceberg the size of a country breaks away, what happens next?

Adrian Luckman, Professor of Glaciology and Remote Sensing, Swansea University

This article was originally published on The Conversation. Read the original article.

0 Responses to “I’ve studied Larsen C and its giant iceberg for years – it’s not a simple story of climate change”

  • I’m surprised that Adrian Luckman is surprised by the level of interest in this calving event. The Antarctic Peninsula is one of the fastest-warming regions on earth and previous ice shelf collapses (further north, and others on the west coast) have been linked to global warming. Understanding and predicting future changes is really important! That is why people are interested. The author’s position seems to be that there is no climate change link unless it can be definitively established for this location considered in isolation. In fact, we know the region is warming, and want to understand the impact of that warming.

    In the penultimate sentence he links to an article in Science, which he says states that Larsen C has been thickening. In fact that article states that Larsen C has been THINNING:

    “Volume loss from Antarctic ice shelves is accelerating”, Paolo et al Science, 2015: “On the eastern side of the Antarctic Peninsula… the regional ice-shelf thinning rate of 3.8 ± 1.1 m/decade is about half of that on the western side. The onset of thinning for Larsen C has progressed southward, which is consistent with climate-driven forcing discussed in earlier studies. The highest thinning rates on Larsen C (with local maximum thinning of 16.6 ± 8.1 m/decade) are near Bawden Ice Rise.”

    The Bawden Ice Rise is exactly where the iceberg finally detached.

    • Adrian Luckman is gunning for 15 minutes of fame at the expense of a huge teachable moment about climate change. He fancies he knows more about climate change than atmospheric physicists because well, he’s a geologist. Never have I seen such a grotesque insertion of self in media messaging. Except for those other 15 scientists who love to claim there’s a debate about cliamte change. Ugh. Just ugh.