Scientists scramble to harvest ice cores as glaciers melt
Scientists are racing to collect ice cores – along with long-frozen records they hold of climate cycles – as global warming melts glaciers and ice sheets. Some say they are running out of time. And, in some cases, it’s already too late.
Late last year, German-born chemist Margit Schwikowski and a team of international scientists attempted to gather ice cores from the Grand Combin glacier, high on the Swiss-Italian border, for a United Nations-backed climate monitoring effort.
In 2018, they had scouted the site by helicopter and drilled a shallow test core. The core was in good shape, said Schwikowski: It had well-preserved atmospheric gases and chemical evidence of past climates, and ground-penetrating radar showed a deep glacier. Not all glaciers in the Alps preserve both summer and winter snowfall; if all went as planned, these cores would have been the oldest to date that did, she said.
But in the two years it took for the scientists to return with a full drilling set-up, some of the information that had been trapped in the ice had vanished. Freeze-thaw cycles had created icy layers and meltwater pools throughout the glacier, what another team member described as a water-laden sponge, rendering the core useless for basic climate science.
The sudden deterioration “tells us exactly how sensitive these glaciers are,” said Schwikowski, head of the analytical chemistry group at the Paul Scherrer Institute in Villigen, Switzerland. “We were just two years too late.”
Extracting ice cores
The U.S. Ice Drilling Program, a federally funded organization established by the National Science Foundation, recommends manual drills to obtain shallow ice cores and motor-powered drills for greater depths.
The mission on Grand Combin underscores the major challenge scientists face today in collecting ice cores: Some glaciers are disappearing faster than expected. The realization is prompting renewed urgency, causing those who specialize in harvesting ice cores to accelerate missions, rethink where to target next, and expand storage capacity.
Almost all of the world’s glaciers are shrinking, according to the United Nations. In its most comprehensive climate report to date, published in August, the UN concluded that “human influence is very likely the main driver of the near-universal retreat of glaciers globally since the 1990s.” The report also said that without immediate, large-scale action, the average global temperature will reach or exceed 1.5 degrees Celsius above the preindustrial temperature average within 20 years.
The pace at which glaciers are losing mass is also increasing. A study published in April in the science journal Nature, found glaciers lost 227 gigatons of ice annually from 2000 to 2004, but that increased to an average of 298 gigatons a year after 2015.
Glaciers have lost 298 gigatons of ice a year since 2015, a study found, which equates to around 0.8 gigatons per day on average. This amount of ice would fill New York City’s Central Park and stand 273 meters (896 feet) high.
About 10% of the land area on earth is currently covered with glacial ice, according to the National Snow and Ice Data Center in Boulder, Colorado. If a glacier is melting and no longer accumulating snow, it means it also isn’t capturing atmospheric gases from today for scientists to study in the future.
Alps’ retreating glaciers
Glaciers in the Alps have been shrinking for decades, according to a database compiled by the Global Land Ice Measurements from Space (GLIMS), an international project to map the world’s glaciers. The Corbassiere Glacier shrank by 30% between 1850-2015.
For Schwikowski, the disappearance of glaciers isn’t just a professional blow; it’s an emotional hit, too. “The mountains look different without them, barren,” she said. In the Alps, the mountains without glaciers are “absolutely frightening.”
How ice reveals climate records
Scientists measure isotopes trapped in ice cores. Those atomic variations within water molecules are like a snapshot of the atmosphere’s composition at the time they were frozen.
The European Project for Ice Coring in Antarctica (EPICA), a program developed in collaboration with the European Commission, conducted deuterium isotope tests in thousands of ice cores to reconstruct climate records from the last 800,000 years.
An example of data collected in ice cores
Here are some key events from the last 800 millennia, based on the findings of the EPICA. The higher the concentration of CO2 in the atmosphere, the higher the earth’s temperatures are. In general, higher temperatures mean more isotopes in the ice.
Last September, Schwikowski stood bundled in snow gear as wet cylinders of ice were winched out of the boreholes on Grand Combin. The wetness surprised her, she said. Frigid meltwater drained from ice core pieces that should have been solid. And the core, which should have been translucent, had sections that were perfectly clear.
Ice cores like those from Grand Combin have helped scientists illustrate humanity’s impact on earth’s climate by providing a record of greenhouse gases dating back well before industrialization. The ice preserves tiny air bubbles – direct evidence of past atmospheres. Ice also captures air pollutants, pollen and other temperature and precipitation measures in a single archive, all on the same time scale, sometimes at the resolution of individual seasons.
What’s in ice cores?
All ice cores are unique in some way. Some are crystal clear, others are opaque with irregular or darker layers. Here are some of the most common characteristics of ice cores.
Another member of the Grand Combin expedition, Italian climate scientist Carlo Barbante, said the speed at which the ice on the Alpine massif had melted in the last few years was “much higher than it was before.” Finding the wet cores was a “complete shock,” he said.
As a result, Barbante and other scientists - including Schwikowski - sped up plans to extract a core from the Colle Gnifetti glacier on the summit of the Alps’ Monte Rosa, a few hundred meters higher than Grand Combin. In June, several months earlier than originally scheduled, they launched. The two cores they drilled were of good quality, Barbante said.
Barbante said he is also hoping to organize a trip to Mount Kilimanjaro, Africa’s highest mountain and the only possible ice core site left on the continent, next year or the year after. One study cited in the recent UN report calculated that present-day warming has already set in motion melting that will eliminate all glaciers on the mountain by 2060.
A 2009 discovery by American scientist Douglas Hardy of the mummified remains of a 19th century pig on one of the highest points of the mountain’s glaciers suggests some of the climate history the scientists are hoping to retrieve is already gone. “The implication of that is that we’ve lost [the] last 200 years’ worth of recorded time,” said Hardy.
Glaciers on Mount Kilimanjaro
Satellite images from the European Space Agency show how ice on Africa’s highest mountain has shrunk compared with three years earlier.
Barbante and Schwikowski are part of a scientist-led group called Ice Memory that is trying to build an archive of ice cores from glaciers around the world. Ice Memory is endorsed by the UN’s main cultural agency, the United Nations Educational, Scientific and Cultural Organization (UNESCO).
So far they have drilled in Europe, Bolivia and Russia. The cores are temporarily being stored in Europe, but the plan is to ship them to Antarctica for long-term storage because the site wouldn’t depend on power, which could suffer an outage.
“A hundred years from now, when the Alpine glaciers will be completely disappeared, we will have the samples” for the future generations of scientists, said Barbante.
Where do ice cores come from?
Below are some of the drilling sites documented by the U.S. National Oceanic and Atmospheric Administration (NOAA).
EXPANDING ICE STORAGE
Beyond greenhouse gases, scientists say they may also be able to use ice cores to study the DNA of ancient bacteria and viruses that could reemerge as the world warms. Frozen insects and plant pollen could also reveal histories of the world’s forests and their fire cycles.
Another team of scientists, whose findings were published in July in scientific journal Microbiome, found viruses nearly 15,000 years old in two ice core samples taken from the Tibetan Plateau in China. The findings identified genetic codes for 33 viruses, at least 28 of which were new to scientists.
That team of scientists included U.S.-based ice core paleoclimatologists Lonnie Thompson and Ellen Mosley-Thompson, who are husband and wife.
Lonnie Thompson said the speed at which ice is disappearing has driven plans to expand his ice core storage facilities at Ohio State University, which he began fundraising for last year. He hopes to raise $7 million. So far he has raised about $475,000 through donations and pledges, according to the school’s Byrd Polar and Climate Research Center. The renovation will double the facility’s storage capacity to more than 13,550 meters of ice cores.
Some of the cores Thompson and his team have collected are the only remaining ice from some glaciers. Two of the six ice core sites on Kilimanjaro in Africa that his team drilled back in 2000 have disappeared. So have sites they drilled in 2010 in Papua, Indonesia. Others will likely be gone within 50 years, said Thompson.
In some of the cases, lakes formed on the glaciers’ surfaces as the ice melted, a red flag that indicated melting could be faster than models previously predicted. He said it was a wakeup call that cores needed to be harvested as soon as possible.
“Ice has a wonderful archive of not only the climate, but also the forcings of climate,” or major causes of climate change, Thompson said. “Those histories are at risk as the earth warms and the glaciers retreat.”
A previous version of the chart titled “An example of data collected in ice cores” inaccurately plotted CO2 and deuterium data on the X-axis resulting in a misleading timeline of events. The X-axis and accompanying captions and annotations have been corrected.
Cassandra Garrison and Clare Baldwin
Simon Scarr, Katy Daigle and Cassell Bryan-Low
National Research Council of Italy; Ca’ Foscari University of Venice; U.S. Ice Drilling Program (IDP); Global Land Ice Measurements from Space ( GLIMS ); U.S. National Science Foundation Ice Core Facility (NSF-ICF); U.S. National Oceanic and Atmospheric Administration (NOAA); European Project for Ice Coring in Antarctica (EPICA); Carbon Dioxide Information Analysis Center (CDIAC); European Space Agency (ESA); Lucas Borges da Silva, University of Bern.