The history of early polar ice cores

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Abstract

The scientific knowledge of the Greenland and Antarctic ice sheets, and the subsequently derived Earth history, has been greatly increased during the past 50 years. Much of the new information was obtained from various studies made on a relatively small number of deep (300–400 m) and several very deep (some over 3000 m) ice cores, recovered from the inland regions of both ice sheets, by different national and international research teams. The beginning, development, and progress of deep polar ice core drillings and core studies is reviewed from the incipient pit study made by Ernst Sorge in 1930, through the trying efforts of three separate international core drilling projects mounted around 1950. The paper continues with a broad overview of the early role and achievements made by two related US Army Corps of Engineers research laboratories: the Snow, Ice and Permafrost Research Establishment (SIPRE), and the Cold Regions Research and Engineering Laboratory (CRREL), from the early-1950's to the late-1980's. International partnerships of CRREL with the University of Copenhagen, Denmark (1966), and the University of Bern, Switzerland (1962), established the foundation of polar ice core science.

Introduction

“Snowflakes fall to Earth and leave a message-----”

Henri Bader (1907–1998)

Modern ice core drilling technology, and the following ice core science studies, were initiated by the US Army Corps of Engineers in the early 1950's, just before the International Geophysical Year (IGY) program began, under the formulation and leadership of Henri Bader, Chief Scientist of SIPRE, in association with his research Branch Chiefs, B. Lyle Hansen, James A. Bender, W. Keith Boyd, Robert W. Gerdel, Robert W. Waterhouse, William H. Parrott, and others. During 1956–1959, the full span of the IGY's, field work, SIPRE successfully recovered the first deep ice cores ever obtained, and suited for integrated scientific study, from both the inland regions of the Greenland and Antarctic ice sheets. In 1961, SIPRE united with the US Army Arctic Construction and Frost Effects Laboratory (ACFEL) to form one laboratory, the US Army Cold Regions Research and Engineering Laboratory (CRREL), and Bader retired and joined the faculty at the University of Miami, FL. CRREL continued with the ice core research base established by SIPRE, and in 1966 and 1968, succeeded in obtaining the first very deep ice cores that penetrated the entire vertical dimensions of both the inland regions of the Greenland and Antarctic ice sheets.

Together, SIPRE and CRREL amassed nearly forty years of research experience and achievements in deep polar ice core drillings and core analyses on a large-scale, and established the fundamental drilling technology for retrieving deep ice cores for climatologic archives. At the beginning, and for more than a decade, SIPRE/CRREL was solely responsible for establishing, defining and developing the entire US ice core drilling research program. In addition, the US Army Corps of Engineers, 1ST Engineering Arctic Task Force (1st EATF) Lt. Col. Elmer F. Clark, Commanding Officer; Capt. Ray S. Hansen, Executive Officer, provided the complete field support required for SIPRE's research on inland Greenland during the pre-IGY, in 1956 and 1957. This included all aspects of logistics, air and surface transportation, communications, field camp construction, and living accommodations. The US Navy Air Development Squadron, VX-E 6; and the Navy's Seabee support component, performed similar logistical services in Antarctica during the 1957–1959 IGY period. The construction of Camp Century, Greenland, an experimental nuclear powered, beneath-the-snow-surface, year-round, 200-person living facility, was completed in 1959 by the Corps of Engineers, Polar Research and Development Center (PRDC), Col Robert J. Giesen, Commanding Officer. The Corps also fully supported CRREL in its first, post-IGY bedrock-drilling project at Camp Century, Greenland from 1960 to1966. Thereafter, the US Navy fully supported CRREL again at Byrd Station, Antarctica, in its first to bedrock-drilling project there from 1966 to 1968.

Around the mid-1960's, CRREL entered into strong international laboratory and field research collaborations with the University of Copenhagen, Denmark, and the University of Bern, Switzerland, as well as with other US and foreign universities and institutes. Dr. Chester Langway participated in and was responsible for developing the SIPRE/CRREL field and laboratory ice core research program; the core sample storage responsibilities; and the scientific redistribution of ice core samples for external studies, from 1957 to 1975 (Langway, 1958a, Langway and Hansen, 1970). During his last nine years at CRREL he also served as Chief, Snow and Ice Basic Research Branch. In 1975, Langway accepted a faculty position and Chairmanship of the Department of Geology at the University at Buffalo (State University of New York), where he continued his active ice core research activities; and with the agreement of CRREL and the authorization of the NSF, accepted the responsibility for the curatorship of all ice cores recovered by the US deep drilling program at the University at Buffalo, for the next 17 years.

Section snippets

Pit studies

The original inspiration to probe into the deep interior of ice sheets started to evolve in Greenland and Spitzbergen in the early 1930's with the original pit studies by Ahlmann, 1933, Ahlmann, 1935, Sverdrup (1935), and especially following the path-breaking research made by Sorge, 1933, Sorge, 1935, during the Alfred Wegener Expedition to central Greenland in 1930–1931 (Schwarzbach, 1986). Sorge was the first to systematically and quantitatively study the near surface snow/firn strata in a

Previous ice core research

It was nearly twenty years after Eismitte before the seeds of interest planted by Sorge's important research results were seriously acted upon. The next step in the saga began, around 1950, almost simultaneously; by three separate international research teams, mounted at three distant global locations, using three different mechanical ice core drilling rigs. One was during 1949–1952 by members of the Norwegian–British–Swedish Antarctic Expedition (NBSAE) (Swithinbank, 1957). They cored to

International Geophysical Year

The early 1950's was a time of renewed and stimulated interest in international polar latitude research, by the marking of the Third International Polar Year activities (IPY), for 1957–1958; soon renamed the International Geophysical Year (Bader, 1958, Crary et al., 1962, Korsmo, 2007b). At long last, the neglected and long overdue research areas in the high latitudes, in some of the most distant, desolate and inhospitable regions on Earth, would be targeted and sponsored, by every nation

Post-IGY bedrock cores

The overall successes of SIPRE's core drillings and early core analyses in Greenland and Antarctica during the IGY programs received widespread interest and approval. The US National Academy of Sciences/Committee on Polar Research (NAS/CPR) adjudged the results significant and meriting their highest recommendation for SIPRE to develop a post-IGY deeper ice coring system capable of reaching bedrock depths (Gould, 1970). The international glaciological community also took favorable notice of

Laboratory analyses

The multidisciplinary laboratory analyses of the Camp Century ice core continued in the fall of 1966; soon after the entire ice core shipment from Greenland arrived at CRREL, Hanover, NH. Ever since the ice core research program evolved and expanded, Langway reached out to other US (19), and foreign (9) scientists or institutions to encourage and solicit new research expertise, especially with researchers having established laboratories in critically important fields of research not available

Greenland Ice Sheet Program

In the early spring of 1970, a group of scientists and engineers from the United States, Denmark, and Switzerland gathered to discuss the possibility of conducting a new major ice core drilling investigation of the entire Greenland ice sheet. Based on their accumulated research experience, acquired by successfully working together for several years; they debated the possibility and benefits to be gained by pooling their field and logistical bases, science specialties, and laboratory facilities,

Paleoenvironmental data

The scientific results of the first deep ice cores recovered from around 300 m to 400 m, and the very deep ice cores, from 1388 m, 2164 m, and 2037 m, have yielded unique windows to past events on Earth, and provided the foundation by which many nations have since drilled deep ice cores in both polar regions. The ice core records also have impacted on a wide spectrum of other scientific disciplines (e.g. geophysics, oceanography, geology, meteorology, climatology, and anthropology), and provide

Conclusions

The successful recovery of the early ice cores during the IGY era advanced a new approach to expose the unknown third dimension of polar ice sheets, and marked a turning point: That embedded within the interior bodies of polar ice sheets were important and fresh secrets of Earth's history, and these new physical and chemical analyses could reveal them. Ice cores opened a new portal to the past, unsealing continuous longtime pre-historical and geological age records of precipitation, climate,

Summary

Deep polar ice cores were first successfully recovered and studied from Site 2, Greenland, in 1956 and 1957; by the US Army Snow, Ice, and Permafrost Research Establishment (SIPRE); and followed by two others from Antarctica, at Little America V on the Ross Ice Shelf in 1958/59; from and Byrd Station, in 1957/58, ranging in depth from 264 m to 411 m. These cores were acquired as part of SIPRE's contribution to the US's polar latitudes research activities conducted during the Third International

Acknowledgements

The renewed pursuit to recover deep ice cores began and succeeded during the IGY, under the visionary foresight of Henri Bader, and the engineering inventiveness of B. Lyle Hansen; and in doing so, introduced a new, and still emerging field of polar ice core science. A.P. Crary (Bert), distinguished polar researcher, and Chief Scientist of NSF's Division of Polar Programs during the difficult early days of this research, was a lasting pillar of dedicated support and encouragement. Full

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