Enter the past:  The DC-3, or C-47 military variant, is intermediate in size and range between the Hercules and Twin Otter, and is one of the few types of aircraft that can be fitted with skis.  The first plane to land at the south pole was a C-47.  However, all of the existing airframes are very old and not suitable for sustained operations of the type we need for scientific exploration.  Fortunately, a company in Wisconsin gives these airplanes a second life by completely restoring them from the bare frame, adding more powerful and safe turbine engines, new electrical and fuel systems, flight instruments, you name it.  They even lengthen the fuselage by over a meter.  The airplanes are essentially new when they roll out of the facility.

The LC-130 Hercules (left) and C-47 (right).

Our project saw the need for such an aircraft and undertook the modification of one to conduct long-range airborne surveys in Antarctica and Greenland.  Last season in Antarctica we proved its capability by surveying a vast, largely unknown part of East Antarctica using fuel and facilities at the coastal stations of McMurdo (US), Casey (Australia), and Dumont d’Urville (France).  We made two stops at Concordia Station (French/Italian) in the interior and obtained about two dozen barrels of fuel there, but that was the only interior resource we used.  We were also able to pack up and move ourselves between these stations while conducting surveys along the way.  This is a first, and has opened the door to a new era of Antarctic exploration.

I have included some video of our unique aircraft and team members in action.  In the next installment I’ll explain a bit about radar and show you some data that we’ve acquired here, since that provides the first and best picture of what is below the ice.  Stay tuned.

This one-of-a-kind airplane features an array of instruments for studying the East Antarctic Ice Sheet and the bedrock below: radar, a magnetometer, laser altimeters, and a gravity meter. Skis allow the team to land nearly anywhere in Antarctica if necessary.

The specially-quipped C-47 aircraft is designed to conduct long-range airborne surveys in Antarctica and Greenland.

The East Antarctic Ice Sheet is the sleeping giant of the cryosphere: it covers more than 95% of the Antarctic continent and locks up more than 60% of the world’s supply of fresh water. Considered much more stable than its smaller counterpart in West Antarctica, scientists are turning more attention to studying the history, structure and dynamics of this mysterious icy world. Instead of taking the stability of the ice sheet for granted, scientists from many different countries are digging into East Antarctica’s climate history to help predict how this vast ice sheet could respond in a warming world.

Graduate students Dusty Schroeder (foreground) and Jamin Greenbaum (rear) monitor instruments during a survey flight.

As a member of a research group at the University of Texas, Austin, Jack Holt participated in a multinational project called ICECAP to survey an enormous, unexplored part of the East Antarctica Ice Sheet. Building on their research experience of the last two decades, the UT team employed a ski-equipped aircraft outfitted with unique instrumentation, including an ice-penetrating radar capable of mapping the surface, internal layers, and the bottom of the ice. Other instruments revealed information about the density and type of the underlying rocks. The aircraft was also fitted with a suite of secondary instruments including specialized GPS receivers and cameras. One of the goals of ICECAP was to find the oldest ice on the continent, the site of a future ice-coring project to unlock climate records that go back a million years.

Data from the ICECAP project will help scientists understand how the East Antarctic Ice Sheet, with its enormous supply of fresh water, might react to changing environmental conditions. The ice in the target area is generally over 2 miles (3.5 km) thick and the bedrock lies mostly below sea level, making this ice potentially more likely to make a rapid contribution to sea level rise than the ice sheets in Greenland or West Antarctica. But the largely unknown continent buried beneath is also important for forecasting how the ice might respond to a warming world: The slope and roughness of the ground, the presence of water (including subglacial lakes), and the type of rocks are all factors.

ICECAP season 1 flight lines.

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.