The history of early polar ice cores
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
References (127)
- et al.
The Camp Century 10Be record: implications for long-term variations of the geomagnetic dipole moment
Nuclear Instruments and Methods in Physics Research
(1984) - et al.
Dating Greenland firn-ice cores with Pb-210
Earth and Planetary Science Letters
(1966) - et al.
Artificial radioactivity reference horizons in Greenland firn
Earth and Planetary Science Letters
(1966) - et al.
Global and local influences on the composition of snowfall at Dye 3, Greenland: the record between 10 ka B.P. and 40 ka B.P.
Earth and Planetary Science Letters
(1985) - et al.
Search for aluminum-26 in dust from the Greenland Ice Sheet
Geochimica et Cosmochimica Acta
(1965) - et al.
Radiocarbon dating of ice
Earth and Planetary Science Letters
(1966) - Ahlmann, H.W. son, 1933. Glaciology, Scientific results of the Swedish–Norwegian Arctic Expedition, 1931, Geografiska...
- Ahlmann, H.W. son, 1935. The stratification of the snow and firn on Isachsen's Plateau, scientific results of the...
Sorge's law of densification of snow on high polar glaciers
USA SIPRE Research Paper
(1953)United States polar ice and snow studies in the International Geophysical Year, in Geophysics and the IGY
Scope, problems, and potential value of deep core drilling in ice sheets
USA CRREL Special Report
Excavations and installations at SIPRE Test Site, Site 2, Greenland
USA SIPRE Technical Report
Temporal variations in the 10Be concentration levels found in the Dye 3 ice core, Greenland
Deep drilling in Antarctica. Colloque sur la Glaciologie Antarctique
Physical investigations on the snow and firn of northwest Greenland 1952, 1953, and 1954
USA CRREL Research Report
Stratigraphic studies in the snow and firn of the Greenland ice sheet
USA CRREL Research Report
Information on the CO2 cycle from ice core studies
Radiocarbon
Climate Crash: Abrupt Climate Change and What It Means to Our Future
Interhemispheric comparison of changes in the composition of atmospheric precipitation during the Late Cenozoic Era
The chemistry of 700 years of precipitation at Dye 3, Greenland
The United States glaciological researches during the International Geophysical Year
Journal of Glaciology
One thousand centuries of climate record from Camp Century on the Greenland Ice Sheet
Science
Ice cores and paleoclimatology in radiocarbon variations and absolute chronology
Climate record revealed by the Camp Century ice core
Frozen Annals: Greenland Ice Sheet Research
A new Greenland deep ice core
Science
Oxygen-isotope studies
Antarctic ice sheet stable isotope analyses of Byrd Station cores and inter-hemispheric climate implications
Science
Changes in precipitation chemistry at Dye 3, Greenland
Journal of Geophysical Research
Drill-hole measurements and snow studies at Byrd Station, Antarctica
The inner structure of the Ross Ice Shelf at Little America V, Antarctica, as revealed by deep core drilling. General Assembly of Berkley
Deep core studies of the accumulation and densification of snow at Byrd Station and Little America V, Antarctica
Preliminary results of studies of ice cores from the 2164 m deep drill hole, Byrd Station, Antarctica
Volcanic ash in the Antarctic ice sheet and its possible climatic implications
Radioglaciology Soundings at Proposed Drill Sites. Technical University of Denmark, Laboratory of Electromagnetic Theory, Report D185
New equipment for radio-echo sounding
Antarctic Journal of the United States
Layer echo's in polar ice sheets
Journal of Glaciology
A battery powered, instrumented deep ice core drill for liquid filled holes
Past volcanism revealed by Greenland Ice Sheet impurities
Nature
Acidity of polar ice cores in relation to absolute dating, past volcanism, and radio echoes
Journal of Glaciology
Greenland ice sheet evidence of post-glacial volcanism and its climatic impact
Nature
Ice-core dating of the Pleistocene/Holocene boundary applied to a calibration of the 14C time scale
Radiocarbon
80,000 years of recorded global volcanism
Climate Change
Deep core drilling and core analysis at Camp Century, Greenland, 1961–1966
Deep core drilling in ice
Cited by (20)
Effect of nanosilica on simethicone-based fluids for drilling in warm ice layer of polar regions
2024, Geoenergy Science and EngineeringThe effect of water cooling conditions on the mechanisms of porous ice formation
2021, International Journal of Heat and Mass TransferCitation Excerpt :At the same time, the investigation of water solidification process and characteristics of the formed ice is of separate interest, in particular, in food industry, biology, and medicine [21–23], cosmology [24], and also in biogeochemistry and ecology [16–25]. For example, the structure of porous sea ice and its gas permeability [26–30] affect the balance of oxygen and greenhouse gases in the Arctic and Antarctic, and also the climate changes at large, while the analysis of gas fractionation in the ice formation is used in paleoecology [31–36]. Recently, the study of ice formation in the presence of dissolved gases has also been carried out in microsystems, when not only the bulk properties of the liquid become significant, but also its interaction with the hydrophilic, hydrophobic, or heterogeneous surface of the vessel in which it is located [37–39].
Hot-water coring system with positive displacement motor
2020, Polar ScienceCitation Excerpt :HWD technology has been extensively used in glaciological investigations with excellent results and high reliability, except for its limitation when used for non-core drilling. In fact, subglacial cores are of importance since these cores provide opportunities for understanding the interplay of dynamic processes of the Earth (Talalay and Pyne, 2017) and reconstructing biological evolution and paleoclimatic and global environmental changes (Langway, 2008). New coring devices must be devised in combination with a HWD system for obtaining core samples from particular depths that might be of scientific interest or for drilling through formations such as rocks and ice tills.
Perennially and annually frozen soil carbon differ in their susceptibility to decomposition: Analysis of Subarctic earth hummocks by bioassay, XANES and pyrolysis
2014, Soil Biology and BiochemistryCitation Excerpt :Four earth hummocks were excavated to the depth of the permafrost using a shovel so that the vertical face exposed one complete cycle of the surface micro-relief patterns (usually less than 2 m wide) in the active layer. A gas-powered SIPRE (Snow, Ice, and Permafrost Research Establishment, Langway, 2008) corer was used to sample below the permafrost table. The soil profiles were described according to the Canadian System of Soil Classification (Soil Classification Working Group, 1998) and sampled in bulk from genetic horizons.
Local environmental changes recorded by clay minerals in a karst deposit during MIS 3 (La Chauverie, SW France)
2011, Quaternary InternationalCitation Excerpt :Global paleoclimatic changes are classically referred to δ18O isotope record from ice accumulated in polar zones (Raymo et al., 2006; Chester and Langway, 2008; Sellén et al., 2008; Villa et al., 2008).
Design and performance of the Hotrod melt-tip ice-drilling system
2023, Geoscientific Instrumentation, Methods and Data Systems