An Antarctic lake suddenly disappears

Side-by-side images of an Antarctic lake with ice-covered water, right side water drained.
A before and after comparison of the ice-covered lake on Antarctica’s Amery Ice Shelf shows blue around the edges of the ice where the lake peeks out on the left. On the right side, the water has drained and the ice above has crumpled and flexed in response. The images here were taken by Landsat 8 during the daylight hours of summer in 2019. Image via Landsat 8/ UC San Diego.

Now you see it, now you don’t

Scientists saw an ice-covered lake atop the Amery Ice Shelf in Antarctica in April 2019. But by June of that year it had drained away, leaving behind a doline – a crater-like sinkhole with the fractured remains of the ice cover – where the lake had once been. The scientists believe the weight of accumulated meltwater created a large fissure beneath the lake, which drained in June in what they said was a “rare event.”

The team of scientists published their study in the peer-reviewed journal Geophysical Research Letters on June 23, 2021. Lead author Roland Warner of the Australian Antarctic Program Partnership at the University of Tasmania said:

We believe the weight of water accumulated in this deep lake opened a fissure in the ice shelf beneath the lake, a process known as hydrofracture, causing the water to drain away to the ocean below.

Hydrofracture is a fracturing of rock, caused by water, often as it freezes to ice. Scientists have seen hydrofracturing in process on ice shelves in Antarctica. But they hadn’t seen it on such a large ice shelf. The Amery Ice Shelf, where this lake once stood, is 4,590 feet (1,400 meters) thick.

How to see in the dark of polar winter

The Amery Ice Shelf is located at 69 degrees south. June is wintertime in the Southern Hemisphere, when it’s dark nearly all the time at this ice shelf. In order to see what was happening on the land below, scientists used a green-light laser instrument on NASA’s ICESat-2. It let scientists see in the dark, essentially. The laser sent pulses of light to the surface. The light bounced back, and scientists were able to record the light travel time.

In this way, they could see the disruption on the ice shelf. The surface of the ice fell 260 feet (80 m) when the lake drained. Losing the heavy load of water on top of the ice shelf also made the floating shelf lighter, so the surroundings of the lake rebounded by 118 feet (36 m).

Black lobes on graph show darkness hours in southern winter.
At the location of the Amery Ice Shelf, which is 69 degrees south on the globe, darkness dominates in June, with only a dim twilight peeking through in the middle of the day. Image via

The University of Minnesota’s Polar Geospatial Center provided maps that showed the disruption also changed the landscape around the newly created doline for 23 square miles (60 sq km).

Helen Amanda Fricker of the Scripps Institution of Oceanography at UC San Diego said:

It’s exciting to see ICESat-2 show us details of processes that are occurring on the ice sheet at such fine spatial scale. Since surface meltwater on ice shelves can cause their collapse, which ultimately leads to sea-level rise when grounded ice is no longer held back, it’s important to understand the processes that weaken ice shelves.

Billions of cubic feet of water lost to sea

Scientists measured the doline that replaced the lake at 4.25 square miles (11 sq km). They estimate that 21 to 26 billion cubic feet (600 to 750 million cubic meters) of water, which is rougly twice the volume of San Diego Bay, drained into the ocean.

Jonathan Kingslake of Columbia University said:

This abrupt event was apparently the culmination of decades of meltwater accumulation and storage beneath that insulating lid of ice.

Simulated aerial view of Manhattan with huge blue cube towering over a portion.
To visualize the amount of water lost on the Amery Ice Shelf, this computer graphic shows the 21 to 26 billion cubic feet of water as a cube atop a portion of Manhattan. Image via Philipp Arndt/ Scripps Institution of Oceanography at UC San Diego.

The uplift from the disruption created a new, shallow lake that refilled during the next melt season in the span of a few days, overflowing into the old doline cavity. When ICESat-2 crossed the doline again a few days later and took more measurements, it found a meltwater channel cut into the doline that was 65 feet (20 m) wide and 10 feet (3 m) deep.

A glimpse of a warmer future

In the future, as warming Antarctic temperatures lead to more surface melting on ice shelves, hydrofracturing will continue to break up ice shelves and therefore drain more water into the oceans and increase the rising sea level. Now researchers have seen that thick ice shelves can also experience hydrofracturing, which must be considered in projections for future warming.

Snow white landscape with dark teal spots and crumpled areas.
The Landsat 8 satellite captured this image of meltwater on the Antarctic Amery Ice Shelf during summer. Image via UC San Diego.

The researchers are unsure about what the future holds for the doline, and whether it will accumulate more meltwater and drain more frequently. In the meantime, they will keep an eye on it.

Bottom line: Years of accumulated meltwater in a lake on the Amery Ice Shelf in Antarctica suddenly drained into the ocean during the winter of 2019.

Source: Rapid formation of an ice doline on Amery Ice Shelf, East Antarctica

Via UC San Diego

June 28, 2021

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