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ARCTIC VOL. 60, NO. 1 (MARCH 2007) InfoNorth Fifty Years of McCall Glacier Research: From the International Geophysical Year 1957–58 to the International Polar Year 2007–08 by Gunter Weller, Matt Nolan, Gerd Wendler, Carl Benson, Keith Echelmeyer and Norbert Untersteiner INTRODUCTION McCall Glacier, located in the eastern Brooks Range of northern Alaska (Fig. 1), has the longest and most com- plete history of scientific research of any glacier in the U.S. Arctic. Spanning the period from the International Geophysical Year (IGY) in 1957–58 to the Fourth Inter- national Polar Year (IPY) in 2007–08, this research has resulted in perhaps the best record of recent climate change and its impacts in this region of the Arctic. Creation of this record played a major role in the lives of numerous people associated with the Arctic Institute of North America and the Universities of Alaska and Washington. This essay attempts to document the history of research on the gla- cier, as well as the evolution of research logistics there, through personal anecdotes from some of the scientists involved. McCall Glacier today is about 6.5 km2 in area and faces mostly north, towards the tundra and the Arctic Ocean coast near Barter Island, Alaska, not far from the Yukon border. The Dictionary of Alaska Place Names (Orth, 1967:607) lists the glacier as follows: McCall Glacier: glacier, heads on Mt. Hubley in Romanzov Mts., trends N 5 mi. to its terminus at head of McCall Creek, 10 mi. E of Mt. Michelson, Brooks Ra.; 69˚20' N; 143˚49' W. Named in 1956 by R.C. Hubley for John Gill McCall, glaciologist, University of Alaska, who died in 1954. John Gill McCall, a World War II veteran, earned his bachelor’s degree in geology at the University of Alaska in 1949 and the first PhD in glaciology ever awarded by Cambridge University four years later. In the fall of 1953, he returned to Alaska to head the Geology Department at University of Alaska Fairbanks (UAF). Known as a glacier expert, he became involved in the rescue of a mountaineer- ing party that had completed the first traverse of Mount McKinley from the southeast side across the peak and FIG. 1 Map showing McCall Glacier and its location in the down the Muldrow Glacier to Wonder Lake. On the de- Brooks Range. Map contours are in meters, based on the scent, the roped-up party fell on a steep ice slope of the 1956 U.S. Geological Survey map. XXX 2 • INFONORTH Muldrow Glacier, where one climber was killed and an- Art Rich (Martin-Marietta), and Untersteiner were flown other badly injured. McCall helped in the evacuation of the to McCall Glacier in a small Cessna by Al Wright, a wounded person, who was left in a tent on the glacier. John renowned bush pilot who looked like Spencer Tracy. After McCall died of polio in 1954, shortly after this event. a smooth landing on the lower, gently sloping part of the glacier, they pitched a tent for the night before making the hike up the glacier to visit Hubley and Mason, who were RESEARCH STARTS DURING already established at the upper station. Hubley seemed THE INTERNATIONAL GEOPHYSICAL YEAR full of energy and enthusiasm and ready to brave the prospect of many months of work in this remote region. As a contribution to the IGY, the Arctic Institute of The next day was spent collecting all the scattered North America, with support from the U.S. Air Force, crates dropped from the air. On the third day, Sater and planned an 18-month study of McCall Glacier. The idea Untersteiner built a rock platform for a truncated Jamesway for this came from Richard Hubley and Walter Wood of hut on the lateral moraine near the lower camp. (Little did the U.S. IGY Glaciological Panel. Hubley was a graduate they realize that this base would be re-used in the late of the University of Washington, having received his PhD 1960s to erect a plywood hut, which survives there to this in 1956 in the Atmospheric Sciences Department, only the day.) The main camp, comprising five half-units of second PhD awarded by the department. Before going to Jamesway huts, was established on the uppermost of the McCall Glacier, Hubley had served as planner and coordi- three cirques of the glacier, with the lower moraine camp nator for the U.S.-IGY Glaciology program in the North- as a secondary location in the ablation area. An emergency ern Hemisphere, working at the National Science retreat camp, another Jamesway hut, was erected on the Foundation (NSF) in Washington, D.C. The initial team on shores of Jago Lake in the foothills, about 15 km from the the glacier included Richard C. Hubley as chief scientist terminus. All of these camps played a role in subsequent (until his death in October 1957), John Sater as junior expeditions. On 13 May, Untersteiner returned to Barter scientist and chief surveyor, Charles Keeler as assistant Island with Al Wright because he had received word that scientist, and Robert Mason as logistics officer and scien- the ice camp in the Beaufort Sea was ready for occupancy. tific assistant. His brief excursion to McCall Glacier was a fortunate and None of the original IGY team members were available memorable event of initiation for a novice to the Arctic. to contribute to this story, but one of us (Norbert In the summer of 1957, Walter Sullivan, the leading Untersteiner) helped with the construction of the glacier science writer of The New York Times, visited McCall camps. In April 1957, reconnaissance flights of the U.S. Glacier to collect material for his book on the IGY, in Air Force Alaska Command had located an ice floe 1000 km which he describes his experiences there (Sullivan, north of Point Barrow that was deemed suitable for the 1961:275–279). He and Dick Hubley discussed the goals establishment of IGY Drifting Station Alpha. The teams of and history of the project. Sullivan found Hubley to be scientists from Columbia University, the University of quiet and, in retrospect, perhaps somewhat preoccupied, Washington, and the U.S. Weather Bureau, including but there was no evidence of the deep-seated trouble that Untersteiner, waited at the former Ladd Air Force Base later led to tragedy. Sullivan even helped with dropping (now Fort Wainwright) near Fairbanks while a crew of supplies on the glacier from a Cessna-180. four civilian construction workers and Air Force person- The weather and climate of the glacier were major nel was preparing the camp for occupancy. At the same topics of the research. Both are influenced by the Brooks time, Walter Wood and his son Peter were also at Ladd Range, which provides a topographic barrier between the AFB, on behalf of the Arctic Institute of North America extreme continental climate of interior Alaska and the (AINA), to coordinate the deployment of two small camps polar climate of the Arctic Basin, with both regimes for Richard Hubley’s IGY project on McCall Glacier. influencing the local glacier climate. The glacier lies As a person with experience working in the mountains, above the prevailing summer stratus cloud decks that Untersteiner was given the chance to help in this glacier cover the Arctic Ocean and extend into the foothills of the deployment. The planes used for this mission were the Brooks Range. It was found that the glacier’s weather was legendary twin-engined C-119 “flying boxcars,” with ample influenced mainly by storms moving over the ocean north cargo space and a cockpit mounted between two slender of the glacier. Storm winds were westerlies but were consid- fuselages. In brilliant weather, they made two flights from erably modified by local topography in the lower sections of Ladd AFB over the snow-covered Brooks Range to the the glacier. Glacier and katabatic winds characterized the glacier, where they pushed boxes with camp and scientific meso-scale circulation between storm periods. gear out the huge cargo door. In total, more than 30 tons of Even during the last glacial maximum, glaciation in the fuel and 18 tons of supplies dropped onto the glacier Brooks Range was never very extensive, since precipita- during the IGY deployment. On the last return flight on 10 tion is relatively low (ca. 500 mm of water, falling largely May, the party landed at Barter Island, where the scientists as snow in spring and fall) and summer temperatures are remained while the C-119 returned to Fairbanks. On the high. Keeler (1959) documented five distinctive advances same afternoon, John Sater and Charles Keeler (AINA), of McCall Glacier. The farthest of these advances gave the INFONORTH • 3 FIG 2. A) A supercub unloads people and supplies in the upper cirque of McCall Glacier, with the IGY camp in the background. B) Main IGY camp on McCall Glacier after a blizzard. Photos by A. Post, AINA. glacier a length of approximately 20 km where it joined a distinguished. Science can as ill afford his loss as can we glacier that used to fill the Jago River valley, compared who knew him as a companion in the office and among the with its 1957 length of about 8 km. Mason studied ice high snows. temperatures and heat flux in the upper cirque of McCall Glacier, in a borehole drilled down to 90 m. While the It was a sad ending after such a promising start. The field upper 15 m showed strong seasonal variations, below that station was closed in October but reactivated in late Feb- level the temperature was fairly constant, with a value ruary 1958 by Keeler, Mason, and Sater, with Sven Orvig close to -1˚C, because of surface meltwater that percolated of McGill University as the new scientific leader of the into the cold firn and refroze, releasing its latent heat.

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