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1975, Arctic
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3 pages
1 file
Researchers are braving the Yukon ever earlier in the season for the Icefield Ranges Research Project (IRRP). The fist group arrived at the IRRP Kluane Lake base camp (61"N, 138'30W) on 15 April 1974 and the last group did not leave until 15 October. The winters of 1974 and 1975 mark the k t occasion of the base camp being open yearround for two consecutive years. This innovation made possible as a result of the appointment of Mr. and Mrs. A. Williams as a resident camp-management team, is necessary scientifically because certain meteorological projects have to be conducted on a twelvemonth basis, as discussed below. One hundred and four researchers and their assistants, representing nearly twenty universities, government agencies and institutions,
ARCTIC, 1977
During 1975 and 1976, research staff and students occupied the base camp of the Icefield Ranges Research Project (IRRP) at Kluane Lake (61"N, 138"30'W) from early April to mid-October. Altogether 126 individuals representing universities and institutes in Canada and the United States made use of the field research facilities during these two years. A decrease from 3,200 mandays of accomodation and subsistence in 1975 to 2,700 in 1976 reflected increasing difficulties in obtaining funds for field research in the North.
Cold War History, 2012
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2009
This is the second article in an occasional series by authors invited to trace how their personal thinking about their research has changed over time.
2017
A field inter-comparison experiment over sea ice was conducted in March-April, 2016 on the sea ice off Qaanaaq, in Northwest Greenland. Six different thermal infrared radiometers participated in the inter-comparison, the first of its kind over sea ice, including two Fiducial Reference Measurements Thermal Infrared Radiometers. The weather conditions were typical for a high Arctic environment, with surface temperatures between -30C and -10C and low wind speeds. Pairwise comparisons of the 10 minute averaged brightness temperatures from the radiometers showed mean differences between 0.13 and 1.0 K and standard deviation from 0.05 to 1.20 K. Inter-comparison of the sky brightness temperatures showed that a lower limit of ~173 K was reached with both FRM-TIR instruments during cold sky conditions. Several other experiments have been conducted during the field campaign, such as spatial variability study, a freeze-up experiment and an angular dependence experiment. All these experiments ...
The northern review, 2023
Reviewed by Glenn Iceton During the onset of the Cold War, the Canadian and American governments engaged in a joint effort to establish weather stations in the High Arctic. Th ese developments occurred concurrently with increased American presence in the Canadian Arctic due to other military endeavours. With some exceptions, northern Canadian historiography examining this era has consequently been characterized by a focus on the American presence in the Arctic and associated sovereignty concerns on the part of the Canadian government. In Th e Joint Arctic Weather Stations, historians Daniel Heidt and P. Whitney Lackenbaur substantially broaden this scope of inquiry. While providing a nuanced analysis of sovereignty issues related to the establishment of Joint Arctic Weather Stations (JAWS)-and, in the process, challenging many previously-held assumptions-Heidt and Lackenbaur also provide numerous insights into the civilian components surrounding the establishment of the weather stations and the logistical challenges faced by planners and station personnel as they attempted to construct and maintain these stations in such harsh environments. Th is broad focus allows the authors to provide significant historiographical contributions not only to diplomatic history, but also to scientific and environmental history. The book is divided into nine chapters. Th e first four chapters are chronologically organized. Chapter 1 focuses on the lead-up to negotiations regarding the establishment of JAWS, setting the context of early meteorological and scientific research in the Canadian North as well as Canadian sovereignty concerns in the decades preceding the Cold War. Chapter 2 discusses the negotiations that ensued between Canada and the United States to allay the former's sovereignty concerns and pave the way for JAWS. The following two chapters discuss the logistics of establishing the first weather stations in the High Arctic and expanding the network of stations.
Arctic, Antarctic, and Alpine Research
The year 2018 marks the 50-year anniversary of Arctic, Antarctic, and Alpine Research (AAAR). During this time period AAAR (formerly Arctic and Alpine Research, AAR) has provided an important outlet for research in cold regions environmental science. AAAR from its inception has been unique for its interdisciplinary nature, publishing papers in a wide diversity of fields including glaciology, geomorphology, paleoceanography, climatology, and ecology. Fifty years ago (1967-1968), the Institute of Arctic and Alpine Research (INSTAAR), with the University of Colorado, undertook a comprehensive plan for expansion. Emphasizing the multi-and interdisciplinary nature of its research, and complementing its existing field station, the Mountain Research Station, INSTAAR added faculty, new courses of study, and graduate mentoring in the environmental sciences with special regard to arctic and alpine regions. A need for a scientific journal covering cold regions research was recognized, and thus Arctic and Alpine Research was created as a component of INSTAAR's expansion plan (Figure 1).
2004
Since the discovery of dung-rich alpine ice patches in southwest Yukon in 1997, continuing multidisciplinary studies have provided a unique window on the biology, climate, and hunting activity in this region over much of the Holocene. Aerial surveys have identified 72 ice patches of variable size, and 65 patches have been ground-surveyed for organic remains. Of these, 35 yielded an abundance of biological specimens, including caribou and other rare large mammal remains, mummified small mammals and birds, and artifacts spanning 8000 years. The dung provides pollen and plant macrofossils for analysis and paleoenvironmental reconstruction, as well as dietary, genetic, and parasitic information. Stratigraphically controlled sampling of dung within ice layers has yielded a geochronology placing their formation as early as 8300 to 8000 years BP. Ice patch formation was nearly continuous except for an interval between 6700 and 4700 years BP and another between 1440 and 1030, when warm or dry conditions (or both) resulted in no net ice accumulation. Resumption of ice accumulation over the following 500 years likely culminated in the Little Ice Age. The size of the ice patches during this period is made evident by a lichen-free zone that haloes each patch. More recently, interpretation of air photos from 1946 to 2001 has found a significant reduction in ice patch dimensions. Daily temperature records for Whitehorse (1942 -2001) were used to calculate melting degree-day values that account for a large part of the variation in ice patch size, indicating that while considerable melting has likely occurred since the end of the Little Ice Age, the ice patches are highly sensitive to decadal changes in temperature.
Titel: Climate …, 2007
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