Antarctica mapped by satellite images. The bedrock below West Antarctica is rising surprisingly fast new research published in Science shows. (Image: USGS, NASA, National Science Foundation, British Antarctic Survey).

The bedrock below West Antarctica is rising surprisingly fast

Thursday 21 Jun 18
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Valentina Roberta Barletta
Post doc
DTU Space
+45 45 25 97 36

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Shfaqat Abbas Khan
Associate Professor
DTU Space
+45 45 25 97 75

An international study lead by DTU


The study published i Science 21 June 2018 is an international cooperation between leading universites lead by The National Space Institue, DTU Space, at the Technical University of Denmark. The study can be found here at www.sciencemag.org.

The other participants are scientists from Ohio State University, DTU Compute/Technical University of Denmark, University of Washington, University of Colorado-Boulder, TU Delft, University of Texas, University of Memphis, Colorado State University, Penn State University and Washington University.

The research is supported by the European Space Agency, ESA, via project GOCE+Antarctica, the U.S. National Science Foundation Office of Polar Programs Antarctic Earth Sciences Program and the U.S. Antarctic Program.

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An international study published in Science and lead by DTU Space finds that the bedrock below the West Antarctic Ice Sheet is rising surprisingly fast which reveals an very fluid Earth Mantle. The findings have implications for the loss of ice at Antarctica.

An international team of researchers, with a new study published in Science with DTU Space as lead author, finds that the bedrock below the West Antarctic Ice Sheet is rising much more rapidly than expected, revealing a very different Earth structure than previously believed. It shows that the Earth Mantle is extremely fluid.

This discovery has important implications in understanding the past, present and future climate changes in Antarctica.

The unexpectedly fast rate of the rising earth may increase the stability of the ice sheet against catastrophic collapse due to ice loss. At the same time the rapid rise, known as uplift, also affects gravity measurements. This implies that up to 10 percent more ice has melted off the West Antarctica Ice Sheet (WAIS) than previously assumed.

“The results of our work will provide a very important contribution in the understanding of dynamics of the Earth along with the ice melting processes in Antarctica,” said leading author of this new study, postdoctoral researcher Valentina R. Barletta at DTU Space, the National Space Institute at the Technical University of Denmark.

 Up to 41 millimeters uplift per year

The Amundsen Sea Embayment (ASE) in West Antarctica alone contributes to 25 percent of all water estimated from melting ice on our planet. To make numbers easier to understand, in one year ASE loses enough to cover an area the size of Denmark (43.000 square km) with a 2.8 meters high layer of ice. The same area (ASE) holds enough ice to potentially raise the global sea level by 1.2 meters or to cover an area the size of Denmark with 11 km of ice.

“The large amount of water stored in Antarctica has implications for the whole planet, but especially for northern Europe”, said Barletta.

"Because of a combination of gravitational effects, surprisingly, the ice lost in Antarctica mostly raises the sea level here, in northern Europe. In contrast, the ice lost in Greenland has no effect here, but it raises the sea level in the southern hemisphere and further destabilizes the WAIS."

The uplift velocity in ASE was measured at up to 41 millimeters per year.

“This is one of the fastest rates of uplift ever recorded in glaciated areas. In comparison, the GPS stations installed nearby the Greenland ice streams record up to 30 millimeters per year, but we know that it is caused by an immediate elastic rebound of the earth, acting like a spring" said Abbas Khan, one of the coauthors and associate professor at DTU Space.

Participating researchers led by scientists at the Ohio State University (OSU) installed a series of GPS stations on rock outcrops around the ASE to measure its rise in response to thinning ice.

“The rapid rise of the bedrock in this part of Antarctica suggests that the geology underneath the ice is different from what scientists had previously believed. The rate of uplift we found is unusual and very surprising. It’s a game changer,” said Terry Wilson, one of the leaders of the study and professor emeritus of Earth Sciences at OSU.

When the ice melts the earth adjusts

Under the massive weight of ice the earth subsides.

“When the ice melts and gets thinner, the earth readjusts, and rises immediately by a few millimeters, which depends on the ice lost," explains Valentina Barletta.

"But the earth also acts a bit like a very hard memory-foam mattress. And it slowly keeps readjusting for several thousand years after the melting. In Scandinavia the bedrock is still rising about 10 millimeters per year because of the last ice age."

Scientists call this delayed readjustment Glacial Isostatic Adjustment (GIA), which can also be described as the Earth retaining memory of the ice lost in the past. How fast this readjustment takes place, depends on the properties of the mantle, the portion inside the earth between the crust and the core that is 2900 kilometers thick.

“Thanks to the satellite observations, we were able to estimate the current ice thinning in ASE, and conclude that the measured uplift rate is up to 4 times larger than expected based on the current ice melting rates”, says Barletta. Therefore the new study focused on the delayed readjustment of the Earth.

Hidden ice loss of up to 10 percent

Valentina R. Barletta has run thousands of GIA simulations using different possible combinations of Earth properties and ice loss scenarios and found that the only way to produce such high uplift is for the Earth mantle to be very fluid (technically low viscosity). These advanced earth simulations are very different from usual ones. To guarantee the reliability of the results under those conditions it was necessary to dig deep into the theory, and also review the codes to prove their correctness and stability without sacrificing the efficiency, essential for processing such an unprecedentedly large variety of simulations. This work was done in close collaboration with DTU Computing Centerwhere all the simulations were run.

"Normally we would see significant uplift happen slowly over thousands of years after the ice age, but here we see it take place in centuries or even decades. This tells us that the mantle below is very fluid and moves quickly when the weight of the ice is taken off," said Barletta.

And the uplift is getting faster. According to this new study, in 100 years, the uplift rates at the GPS sites will be 2.5 to 3.5 times more rapid than currently observed.

Among the direct consequences of this study there is a revised estimate of the ice loss in ASE. When a massive amount of the ice melts it reduces the local gravity and leaves fingerprints that can be measured by satellites and used to estimate the total mass lost. But the earth’s readjustment also produces a gravity change that partially compensates for this loss and hides the ice signal.

“Now we know that in ASE the earth readjusts so fast that 10 percent of the ice loss was hidden, but now we can fix that,” said Barletta.

The earth uplift also works as a feedback 

The fast earth response is potential good news for the future of the WAIS. In this area of Antarctica most of the ice is grounded below sea level, and therefore vulnerable to melting from below by ocean water flowing in underneath the ice sheet. Here the earth uplift works as a feedback that can slow down the ice retreat in different ways.

The uplift raises the so called 'pinning points' – elevated features that pin the ice sheet to the bedrock, preventing the retreat of the grounded ice. At the same time the uplift changes the inland slope of the ground that becomes more effective in holding the ice from sliding away.

In addition, the massive amount of the ice lost reduces the local gravity and the gravitational pull on the water, resulting in a lower sea level at the adjacent Antarctic coast. This in turn reduces the buoyancy of the whole ice sheet, promoting the stability of the ice sheet.

Modeling studies have shown that bedrock uplift could theoretically protect WAIS from collapse, at least in case of moderate climate changes. But it was believed that the process would take too long to have practical effects.

The mantle that we discovered under ASE is more fluid and hotter, and therefore the earth uplifts faster than in the most optimistic hypotheses used in previous studies. “Under many realistic climate models, this should be enough to stabilize the ice sheet,” Wilson said.

But, if future global warming is too extreme, according to the scientists the WAIS will most likely still collapse regardless of stabilizing feedbacks.

"Apart from giving us a new picture of the earth dynamics in Antarctica, the new findings will push to improve ice models for WAIS to get a more precise picture of what will happen in the future” said Barletta.

"They also tell that we clearly need to improve our knowledge of the Earth structure under the whole Antarctic continent. To do so we use GPS in the few areas where they can be installed, and elsewhere we use data from ESA's Earth Explorer GOCE and seismic tomography."

Video. See the Antarctic uplift explaned in 101 seconds:

3 figures explaining the uplift of the bedrock beneath the ice at Amundsen Sea Embayment (ASE) in West Antarctica

Figure 1:

Figure1

Here we see Antarctica (Google Earth view) and a cut to show the interior of the earth, where the mantle (red and dark red) and the core (yellow) are visible.

The Amundsen Sea Embayment (ASE) is indicated by the red rectangle. Note that the largest arrow represents 4.1 cm/yr. Then we can see the photos of four the GPS sites, clockwise from top left: Bear Peninsula (BERP) (Photo Credit: Bill MaGee), Backer Islands (BACK) (Photo credit David Saddler), Inman Nunatak (INMN) (Photo Credit: Jeremy Miner), Lepley Nunatak (LPLY) (Photo Credit: Jeremy Miner).  In the center we can see a zoom over ASE with the measured uplift velocities (black arrows) at the GPS sites. From the left to the right the station code are LPLY, THUR, INMN, BACK, TOMO, BERP. Each photo of GPS site portrais the small mushrom-shaped GPS antenna and the nearby much larger equipment with solar panels. The solar panel are almost vertical because the sun in Antarctica is always very low on the horizon.

Illustration credit: VR. Barletta/Google Earth/David Saddler/Jeremy Miner/Bill MaGee. Illustration text: VR. Barletta.

 

Figure2:

Figure2

This figure (2) is an excerpt from an ESA video-animation explaining the landrise described in the Science article (see the video above, or by clicking here)  

A view from above of Antarctica (A) then zooming in Amundsen Sea Embayment (ASE) and shows the satellites flying over the ice that is thinning.

A portion of the ice and the ocean is then removed to show the bedrock (C) and the GPS locations. The bedrock is then cut to show the crust (brown) the bottom of the lithosphere (grey line) and the mantle (red-orange) pushing up the layer above. In the end we will see the pattern of the uplift rates (D) while it is shown the bedrock uplifting pushed by the mantle. The pattern of uplift rates is provided by V.R. Barletta. The color gradient of the mantle indicates the temperature from hot (bright yellow) to relatively cool (dark red). The mantle temperature and the crustal thickness is derived from GOCE (data from Folker Pappa). The ice thickness and the bedrock topography is from BEDMAP2.

Illustration credit: Planetary Visions/ESA/V.R. Barletta. Illustration text: VR. Barletta.

 

Figure 3:

Figure3

Amundsen Sea Embayment in West Antarctica with the ice sliced to show the bedrock and the earth cut to show the crust (brown) the bottom of the lithosphere (red area) and the mantle (yellow).

The color gradient indicates the temperature from hot (bright yellow) to relatively cool (dark red). In space three satellites are flying; from the right, a GPS satellite, GOCE, which measures the static gravity, and Cryosat2, which measures the changes in ice thickness. The ice thickness and the bedrock data is from BEDMAP2, the mantle temperature and the crustal thickness is derived from GOCE (data from Folker Pappa). 

Illustration credit: Planetary Visions/ESA. Illustration text: VR. Barletta.

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