The Antarctic Peninsula’s retreating ice shelves


The Antarctic Peninsula experienced unprecedented warming during the latter part of the 20th Century. This caused seven floating ice shelves to retreat dramatically with very little of their area now remaining. In recent decades the air temperatures in this region have stabilised, and no further collapses have occurred. The changes give us clues about the impact of climate change across Antarctica in the coming centuries.

What are ice shelves?

Ice shelves are glacial ice; the floating extensions of a grounded ice sheet. Although a few small ice shelves exist in the Arctic, most occupy bays around the coast of Antarctica. The largest ice shelf, the Ronne-Filchner, covers an area slightly smaller than Spain and is up to two kilometres thick. Over many years ice shelves find their natural size when the amount of snow falling on the surface, and the amount ice delivered by glaciers, balances the rate of ice loss through ocean melting and iceberg calving. A change in any of these factors will cause an ice shelf to change its size.

What is happening to Antarctic Peninsula ice shelves?

The long mountainous landmass known as the Antarctic Peninsula has always been warmer than the interior of the Antarctic continent. Each summer produces significant amounts of meltwater on the Antarctic Peninsula’s ice shelves. Each shelf can tolerate only so much meltwater before they weaken and begin to retreat — scientists call this the ‘limit of viability’.

As the climate on the Antarctic Peninsula warmed — by 3°C during 1950-2000 — the limit of viability for ice shelves moved southwards. Ice shelves that used to be stable retreated. Since the warming has stabilised, no further ice shelves have retreated.

How much ice has been lost?

Since the 1950s, a total of 25,000 km2 of ice shelf has been lost from around the Antarctic Peninsula. In volume, this is the equivalent of the UK domestic water requirement for around 1,000 years.

Retreat and collapse?

For some ice shelves, loss of area has occurred progressively over several decades. For others there have been dramatic episodes of collapse. Some progress in determining the exact mechanisms responsible is now being made.

Does this ice loss affect sea level?

The loss of ice from ice shelves has very little direct impact on sea level, but the acceleration of glaciers draining ice from the grounded ice sheet has been reported as a consequence of ice-shelf retreat in several places. Overall, this and other effects are leading the Antarctic Peninsula to contribute about 0.1 mm per year to global sea-level rise. The current total rate of global sea level rise is approximately 3.7 mm per year according to the latest data from the Intergovernmental Panel on Climate Change.

When did we first make the link with climate change?

In 1991, the Wordie Ice Shelf was the first ice shelf to be shown to be retreating. However, it was in 1996, after the retreat of the Prince Gustav and the dramatic break-up of the Larsen-A ice shelves, that BAS first presented evidence that these events were caused by the warming at that time.

Have ice shelves been lost before?

Sea-bed sediment cores indicate that before their recent loss, some ice shelves were present continuously for at least 10,000 years. This suggests that the current ice-shelf retreat, and climate warming, are unprecedented on this timescale and are not solely part of a natural cycle of change.

What does the future hold for Antarctic ice shelves?

If atmospheric warming resumes on the Antarctic Peninsula, it is likely that more ice shelves will be lost in the coming century. Larsen C is the largest ice shelf on the peninsula and restrains the inland flow of many glaciers. While this ice shelf currently appears stable, further climatic forcing could cause it to retreat.

Fact file

  • George VI Ice Shelf — this ice shelf is unusual in that it is constrained within a narrow channel and loses most of it mass to melting, rather than iceberg calving. This suggests that this ice shelf may be most sensitive to changes in ocean conditions, and less sensitive than its neighbours to atmospheric change.
  • Larsen A Ice Shelf — The final-stage collapse of Larsen A in 1995 was a dramatic event that filled the headlines worldwide. The rapidity of the break-up, which occurred in a matter of weeks and left an armada of small icebergs in the Weddell Sea, was unprecedented.
  • Larsen B Ice Shelf — The progression of retreat on this ice shelf was broadly similar to that which occurred on its neighbour Larsen A, but its final collapse did not occur until 2002.
  • Larsen C Ice Shelf — To date, this ice shelf has not shown evidence of climate-driven retreat. An exceptionally large iceberg calved from Larsen C in 2017, but it is not clear that this event was anything other than a natural part of the ice shelf life cycle.
  • Prince Gustav Ice Shelf — This ice shelf retreated progressively through the late-20th century. In 1995, it finally collapsed, leaving open water between James Ross Island and the main Antarctic Peninsula.
  • Wilkins Ice Shelf — This ice shelf collapsed in 2009. Wilkins ice shelf was unusual in that it was fed by very little glacier flow, instead being sustained by its own snowfall.  This made it very vulnerable to atmospheric changes.


On this site: Paul Holland, Oliver Marsh, John King
30 June, 2022