Ice core just coming out of drill.

All of this work is completed in an 8 m (26 ft) deep trench that was painstakingly dug out last year (but with snow blowers…at least not with shovels!). This trench has been covered with a wooden roof (complete with sky lights), and makes for a fairly comfortable, albeit cold for the sake of the ice cores, working environment.

Kaitlin in the science trench.

Descending the steep stairway from the surface into the system of trenches (one trench is for the drilling operation and one is for the science operation) is otherworldly. It really looks like a civilization of trolls has dug themselves a snow palace. Think Lord of the Rings meets North Pole. Connecting the drill trench and the science trench is a wide passageway through the snow, on the other end of which is a marvel of a laboratory. Several stations are set up where different measurements are being made—each station is manned by some of the best and the brightest graduate students around. Unlike most US drilling programs, for this program, a lot of the ice core measurements are being done on site. This eliminates the risk of something happening to the precious cores before the measurements can be made and helps reduce contamination from handling the core. Basically this hole in the snow in the middle of nowhere has been turned into one of the most advanced ice core laboratories in the world.

The well-tuned processing line. We’re jammn,’ mon.

The trenches are cold, yes, but the group working keeps up morale by listening to music (lots of Bob Marley and Jack Johnson…fairly tropical selections) and taking frequent, mandatory tea and coffee breaks. There are too many nationalities (German, French, Japanese, Greek, Danish, Australian, American) in the trench to keep track of, and everyone pitches in to help everyone out, so that no one falls behind and the work continues seamlessly.

The Stations

Atsushi works the Swiss Saw, which cuts the top of the core off to leave a flat surface for measurements.

The Swiss Saw is run by Atsushi from the Low Temperature Institute in Hokkaido, Japan, who happens to be a whiz at the thing, very fast and precise. He is hard to keep up with. The Swiss saw cuts the top of the ice core off, as it is lying down horizontally. This allows for several of the next measurements to be made, as it leaves a nice flat surface to work on.

The line scan. Bubbles in the ice are visible as the line scanner moves over the core.

Vasileois carefully preparing the ice core for the line scan.

The line scan is run by Vasileios from Denmark. The line scanner is a video camera set on a track that records an image of the cores after Vas, and his helper Kaitlin (Kaitlin agreed to help out for a bit in the science trench after we had most of our work done), have carefully shaved the top of the ice core so that it becomes perfectly clear. The line scan records the visual stratigraphy, or layering, in the ice core. The ice core is photographed against a dark background using indirect light, which allows for clear and cloudy bands in the ice to be imaged. The cloudy bands contain more impurities, especially dust, than the clear bands of ice, and show up white while the clear bands show up as black against the background. The bands are indications of seasonal cycles, with dustier ice with higher impurities originating in summer months.

Lars sets up a core in the DEP.

The DEP (Dielectric Profile) is run by Lars from the Alfred Wegener Institute in Bremerhaven, Germany. The DEP is essentially two curved electrodes that are scraped down the top of the ice core (the cut that Atusushi made!) and record the conductivity and the permittivity of the ice which are sensitive to the acidity and the amount of sea salt in the ice. These, in turn, vary with the seasons, and so the DEP can be used to date the ice on a very fine scale.

Aslak runs the ECM.

The ECM (Electrical Conductivity Measurements) is run by Aslak, also from Denmark. The ECM consists of two electrodes, much like the DEP, which are drug down the ice core and record the electrical conductivity of the ice core. The electrical conductivity is sensitive, among other things, to peaks in acidity in the ice core due to volcanic eruptions. Where the electrodes record a peak in conductance is a layer where volcanic material has been deposited. Knowing when the volcano erupted helps then with dating the ice core. Together using the line scan, the DEP and the ECM together is a really powerful way of ensuring that the dating is done in the most accurate way possible…basically there are three independent measures of the annual and sub-annual layers in the ice.

Celebrating 500 m of cores processed in the CFA lab

The CFA (Continuous Flow Analysis) is run by 6 researchers in two shifts, and is really an amazing set up. The CFA essentially melts one section of the core (a “stick” or a rectangular section that has been cut out of the middle of the core by yet another army of science trenchers who man the saws), sucks the flow from the center of the melting ice, discards the waste water from the edges, and feeds the center flow to a series of analyzers which measure the melted ice core water for different chemicals. The concentration of people, instruments, and computers in the DFA lab is enough to produce a lot of heat, so the CFA has been housed in it’s own little insulated space to keep the rest of the science trench cold. The CFA lab reaches temperature of 30 deg C (around 85 deg F)! It’s a funny scene in there, with the 3 researchers in t-shirts while everyone else is bundled up in the science trench.

Physical Properties. Back in her own little room off of the science trench, Daphne of the LGGE in Grenoble, France, measures the size and the orientation of the crystals in the ice.

In addition to the different science stations, a bevy of other researchers works to cut and package the cores. When everyone is down there working together, it resembles an ice core ballet (just well-insulated and heavily clothed)! It really is amazing to watch.

Anaïs prepares sections of core to be shipped to various labs all over the world.

IPY

This Ice Stories Web site was created in celebration of the International Polar Year (IPY) 2007–08, but what exactly is that? The IPY is a large international scientific initiative with a history that spans more than a century.

Portrait of Karl Weyprecht. Photo courtesy of the Alfred Wegener Institute.

The inspiration for the first IPY, held in 1882–83, came from Austrian scientist, explorer, and naval officer Karl Weyprecht. He realized that studying the poles was an important way to understand meteorology and geophysics, but he also knew that it was a big undertaking; it couldn’t be done by one nation alone. Inspired by this idea, a group called the International Polar Commission was established in 1879; it organized the first IPY.

Twelve countries, including the United States, participated; they collectively completed fifteen polar expeditions: two to Antarctica, and thirteen to the Arctic. They probably spent more time trying to survive than they did doing science. There were also problems with countries publishing their own data rather than doing it cooperatively with other nations. But this first IPY was still very valuable. It set in motion the important idea of a collaborative, international scientific effort to study the poles, a spark that rekindled fifty years later.

The Dutch ship Varna got stuck in pack ice in January 1883 during the first IPY. Though the ice crushed the vessel, the scientists were able to continue their research by creating a makeshift observatory on the ice.

American Admiral Richard Byrd created an inland research station as part of the second IPY (1932-33). Photo copyright Ohio State University Archives.

The second IPY (1932–1933) was more scientifically successful than the first. It was proposed and promoted by the International Meteorological Organization as a way to study the newly discovered jet stream (a current of rapidly moving upper atmosphere winds) and its global effects. New inventions—airplanes and motorized sea and land vehicles—made life easier for the scientists. This time, the number of participating nations jumped to forty. Despite challenging economic issues (this IPY took place during the middle of the Great Depression), it brought advances in our understanding of magnetism, atmospheric science, and radio science and technology. Forty permanent observation stations were built in the Artic, and the second U.S.-backed Byrd expedition built the first inland research station in Antarctica.

A 1958 U.S. postage stamp commemorates the International Geophysical Year (IGY).

The second IPY was followed, in 1957–58, by the International Geophysical Year (IGY), a major scientific event that propelled our scientific understanding, particularly of geophysics, far forward. It was proposed by prominent post–World War II physicists, who wanted to use some of the latest technology developed for the war—radar, computers, and rockets—for scientific research, particularly in the upper atmosphere. Sixty-seven countries and more than 4,000 research stations participated.

A member of the U.S. Navy repairs a radio at McMurdo Station during the 1957-58 IGY.

There were many breakthroughs. Important research into continental drift (when the continents change position in relation to each other) was done at this time. The Gambutserv Mountains, a huge completely ice-covered mountain range in East Antarctica, were discovered. Scientists were able to develop the first informed estimates of Antarctica’s ice mass by traversing the continent. The space age was born when the world’s first satellites (the Soviet Union’s Sputnik I in 1957 and the United States’ Explorer I in 1958) were launched. And the Van Allen radiation belts, which encircle the earth trapping cosmic radiation, were discovered. Twenty years later, in 1970, the scientific disciplines emphasized during IGY became the foundation of many of the United States’ National Oceanic and Atmospheric Administration (NOAA) programs and activities.

The twelve nations that were active during the 1957–58 IGY signed the Antarctic Treaty; their flags fly around the ceremonial pole at the Amundsen-Scott South Pole station.

There was also a political outcome to the collaborative work of the IGY. The Antarctic Treaty, written in 1959 and ratified in 1961, states, among other things, that information has to be shared openly among researchers; that science done in Antarctic is for peaceful, noncommercial uses; and that no weapons development or testing can take place there. The Treaty also forbids mineral extraction of any kind and protects the terrestrial ecosystem of Antarctica, which makes it a much different place than the Arctic.

The IPY 2007-08 logo.

The current IPY is, technically, not a year, it’s two (March 2007–March 2009); the two years allow for two full field seasons at both poles. Like its predecessors, this IPY is also a major international, interdisciplinary scientific effort targeted at better understanding the polar regions. Thousands of scientists from over sixty countries, working on over two hundred research projects, are using state-of-the-art tools and techniques to conduct biological, physical, and social research. The goal of this IPY is to explore new frontiers in polar science, improve our understanding of the pivotal role of the polar regions in global processes, and educate the public about the Arctic and Antarctica (that’s where this Web site fits in). Its organizers also hope that this IPY will attract the next generation of scientists and engineers to the poles. The entire worldwide effort is overseen by the International Council for Science (ICSU), and the World Meteorological Organization (WMO).

It’s hard to know what breakthroughs will come from recent data collected, but this IPY has already taken a different kind of leap forward. During the 1957–58 IGY, the majority of countries, including the United States, didn’t allow women to work on The Ice. Now, women account for almost half of all IPY scientists, and many are project leaders. (To learn more about women and the Ice, click here.)

Researchers install GPS devices for POLENET, one of the many IPY 2007-08 projects led by women.