11,348 research outputs found
London 2012 and the impact of the UK’s Olympic and Paralympic legislation: protecting commerce or preserving culture?
The general commercial rights associated with the Olympic Movement are protected in the UK by the Olympic Symbols etc (Protection) Act 1995. In addition, the UK Government, in response to a requirement of the Host City Contract with the International Olympic Committee, created the London Olympic Association Right under section 33 and Schedule 4 of the London Olympic and Paralympic Games Act 2006. These provisions enable the London Organising Committee of the Olympic Games to exploit, to the fullest extent, the commercial rights associated with the London Olympic Games. This article questions whether the IOC’s requirement for legislative protection and state enforcement of the commercial rights are compatible with the Fundamental Principles of Olympism as defined in the Olympic Charter, and its stated aim of being a celebration of sporting endeavour, culture and education
[Review of] Frederick J. Dockstader. The Kachina and the White Man: The Influences of White Culture on the Hopi Kachina Cult
To the delight of scholars of Native American studies and all other readers with even a passing interest in traditional Puebloan cultures of the American Southwest, Frederick Dockstader\u27 s classic study, The Kachina and the White Man, now has been published in a revised and expanded version. This historical narrative of Hopi life, using spirit beings known as kachinas as its central focus, traces the changes and adaptations the Hopi have made in response to pressures placed upon that Indian culture by the seemingly -- inevitable contact with white society. In addition, the author describes in infinite detail the ceremonialism, costuming, masks, and other paraphernalia associated with the colorful Kachina dance rituals, and also discusses the Kachina dolls -- so popular among non-Indian art collectors and museum curators -- and places these figurines in proper cultural perspective, explaining their use in both educating and constantly reminding Hopi children of the religious beings and the appropriate behavior they represent
[Review of] Fred McTaggart. Wolf That I Am: In Search of the Red Earth People
Fred McTaggart\u27s engaging narrative Wolf That I Am: In Search of the Red Earth People is as much a personalized story of self discovery as it is a discussion of surviving Mesquakie folklore. In the early 1970s, as a graduate student at the University of Iowa, McTaggart set out to gather and to analyze the folk stories told among Mesquakies, known historically to the non-Indian world as the combined Indian tribes of the Sac and Fox. Today the main body of this Native American group resides on a tribally-owned settlement (decidely [decidedly] not a government-controlled reservation as mentioned in the foreword) located along the Iowa River in east central Iowa
Wetting on Lines and Lattices of Cylinders
This paper discusses wetting and capillary condensation transitions on a line
and a rectangular array of cylinders using an interface potential formalism.
For a line of cylinders, there is a capillary condensation transition followed
by complete wetting if the cylinders are sufficiently close together. Both
transitions disappear as the cylinder separation is increased. The dependence
of the wetting phase diagram of a rectangular array of cylinders is discussed
as a function of the chemical potential, substrate--fluid interaction strength
and surface tension.Comment: 17 pages in total: 11 pages of Latex document and 6 pages of figures,
Latex Version 2.09, OUTP-93-40
Catalog Maintenance
published or submitted for publicatio
Airborne lidar measurements of El Chichon stratospheric aerosols, October 1982 to November 1982
A coordinated flight mission to determine the spatial distribution and aerosol characteristics of the El Chichon produced stratospheric aerosol was flown in October to November 1982. The mission covered 46 deg N to 46 deg S and included rendezvous between balloon-, airplane-, and satellite-borne sensors. The lidar data from the flight mission are presented. Representative profiles of lidar backscatter ratio, plots of the integrated backscattering function versus latitude, and contours of backscatter mixing ratio versus altitude and latitude are given. In addition, tables containing numerical values of the backscatter ratio and backscattering functions versus altitude are supplied for each profile. The bulk of the material produced by the El Chichon eruptions of late March 10 to early April 1982 resided between latitudes from 5 to 7 deg S to 35 to 37 deg N and was concentrated above 21 km in a layer that peaked at 23 to 25 km. In this latitude region, peak scattering ratios at a wavelength of 0.6943 micron were approximately 24. The results of this mission are presented in a ready-to-use format for atmospheric and climatic studies
Airborne lidar measurements of El Chichon stratospheric aerosols
A NASA Electra airplane, outfitted with a lidar system, was flown in January to February 1983 between the latitudes of 27 deg N and 76 deg N. One of the primary purposes of this mission was to determine the spatial distribution and aerosol characteristics of the El Chichon-produced stratospheric material. This report presents the lidar data from that flight mission. Representative profiles of lidar backscatter ratio, plots of the integrated backscattering function versus latitude, and contours of backscatter mixing ratio versus altitude and latitude are given. It addition, tables containing numerical values of the backscatter ratio and backscattering function versus altitude are supplied for each profile. The largest amount of material produced by the El Chichon eruptions of late March to early April 1982, which was measured by this flight, resided between 35 deg N and 52 deg N. Peak backscatter ratios at a wavelength of 0.6943 micro m decreased from 8 to 10 at the lower latitudes to 3 at the higher latitudes. Backscatter ratio profiles taken while crossing the polar vortex show that the high-altitude material from El Chichon arrived at the north polar region sometime after the winter polar vortex was established. This report presents the results of this mission in a ready-to-use format for atmospheric and climatic studies
Airborne lidar measurements of El Chichon stratospheric aerosols, January 1984
A lidar-equipped NASA Electra aircraft was flown in January 1984 between the latitude of 38 and 90 deg N. One of the primary purposes of this mission was to determine the spatial distribution and aerosol characteristics of El Chichon produced stratospheric material. Lidar data from that portion of the flight mission between 38 deg N and 77 deg N is presented. Representative profiles of lidar backscatter ratio, a plot of the integral backscattering function versus latitude, and contours of backscatter mixing ratio versus altitude and latitude are given. In addition, tables containing numerical values of the backscatter ratio and backscattering function versus altitude are applied for each profile. These data clearly show that material produced by the El Chichon eruptions of late March-early April 1982 had spread throughout the latitudes covered by this mission, and that the most massive portion of the material resided north of 55 deg N and was concentrated below 17 km in a layer that peaked at 13 to 15 km. In this latitude region, peak backscatter ratios at a wavelength of 0.6943 microns were approximately 3 and the peak integrated backscattering function was about 15 X 10 to the -4/sr corresponding to a peak optical depth of approximately 0.07. This report presents the results of this mission in a ready-to-use format for atmospheric and climatic studies
Airborne lidar measurements of El Chichon stratospheric aerosols, May 1983
An experimental survey flight to determine the spatial distribution and aerosol characteristics of the El Chichon-produced stratospheric aerosol was conducted in May 1983. The mission included several different sensors flown abroad the NASA Convair 990 at latitudes between 72 deg. and 56 deg. S. This report presents the lidar data from that flight mission. Representative profiles of lidar backscatter ratio, plots of integrated backscattering function versus latitude, and contours of backscatter mixing ratio versus altitude and latitude are given. In addition, tables containing numerical values of the backscatter ratio and backscattering function versus altitude are supplied for each profile. By May 1983, material produced by the El Chichon eruptions of late March-early April 1982 had spread throughout the latitudes covered by this mission. However, the most massive portion of the material resided north of 33 deg. N and was concentrared below 21 km. In this latitude region (33 deg. N to 72 deg. N), peak backscatter ratios at a wavelength of 0.6943 microns varied between 3.5 and 4.5, and the peak integratred backscattering function was about 18 X 10 to the -4 power/sr, corresponding to a peak optical depth calculated to be approximately 0.08. This report presents the results of this mission in a ready-to-use format for atmospheric and climatic studies
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