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Spiro and Fort Coffee phases changing cultural complexes of the Caddoan area /Rohrbaugh, Charles Lawrence. January 1900 (has links)
Thesis (Ph. D.)--University of Wisconsin--Madison, 1982. / Typescript. Vita. eContent provider-neutral record in process. Description based on print version record. Includes bibliographical references (leaves 240-249).
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Political history of Oklahoma, 1907-1949 /Scales, James R. January 1949 (has links)
Thesis (Ph. D.)--University of Oklahoma, 1949. / Includes bibliographical references (leaves 505-522).
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Coping with limits : responding to reform in Oklahoma /Farmer, Rick, January 1998 (has links)
Thesis (Ph. D.)--University of Oklahoma, 1998. / Includes bibliographical references (leaves 210-216).
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The historical development of the Negro in OklahomaWashington, Nathaniel Jason, 1910- January 1947 (has links)
No description available.
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Manual for the Catalog Dept. of the University of Oklahoma LibraryPotts, Mary Evelyn. January 1956 (has links)
Thesis (A.M.L.S.)--University of Michigan, 1956. Cf. Library literature, 1955-1957, p. 636.
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Manual for the Catalog Dept. of the University of Oklahoma LibraryPotts, Mary Evelyn. January 1956 (has links)
Thesis (A.M.L.S.)--University of Michigan, 1956. Cf. Library literature, 1955-1957, p. 636.
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The structural relationship of economic interest groups to voting patterns Oklahoma 1930-1942 /Harrington, Albert Dale. January 1978 (has links)
Thesis (M.S.)--Wisconsin. / Includes bibliographical references (leaves 139-142).
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The role of Kansas in booming OklahomaHeth, Harold Munn January 2011 (has links)
No description available.
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Survivorship and Breeding Dispersal Patterns of a Migratory, Socially Monogamous Passerine; the Scissor-tailed Flycatcher (Tyrannus forficatus)Becker, Adam John 07 January 2016 (has links)
Survivorship (the likelihood of survival from one year to the next) and breeding dispersal (movement between breeding seasons) exhibit considerable variability at both the inter- and intraspecific levels. Using eight years of data (2008-2015), from my study site in southwest Oklahoma, I characterized survivorship and breeding dispersal of the Scissor-tailed Flycatcher (Tyrannus forficatus) in a mixed-grass prairie ecoregion. My results suggest that estimated survivorship of Scissor-tailed Flycatchers is low, especially to the congeneric Eastern Kingbird (T. tyrannus), and was likely underestimated due to the tendency of Scissor-tailed Flycatchers to disperse long distances.
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An examination of structure and parameterization of turbulence in the stably-stratified atmospheric boundary layerRuscher, Paul Harold 02 October 1987 (has links)
The very stable boundary layer is a region of the atmosphere typified by large
vertical gradients of temperature and momentum. Analysis of very stable atmospheric
flows is complicated by the presence of nonlinear interactions among gravity waves, shear-driven
overturning circulations, two-dimensional vortical modes and intermittent turbulence
in various stages of development. This study examines the horizontal structure of a very
stable atmospheric boundary layer, using data obtained primarily from terrain-following
aircraft flights over central Oklahoma.
Several diagnostic procedures are applied to the aircraft data, including classical and
rotary spectral analysis, principal component analysis, and structure functions. Coherent
structures with sharp boundaries are examined with a new conditional sampling technique
which requires little a priori specification of sampling criteria. Because the flows involve
sharp boundaries, spectral techniques do not provide as much useful information as other
more localized procedures. The edges of the coherent structures are regions of significant
vertical heat transport, a feature not often emphasized in studies of gravity waves and
vortical modes in the stable boundary layer.
The presence of significant turbulence even for large stability has implications for
modelling of the very stable boundary layer. Forecasts of minimum temperature, boundary
layer height, inversion characteristics, and pollutant dispersal are all significantly affected
by turbulent mixing. Many models of the stable boundary layer artificially arrest the
mixing under stable conditions, resulting in, for example, overestimates of nocturnal
cooling. A new parameterization of the stable boundary layer is studied here by
incorporating it into an existing model of the planetary boundary layer. The model is then
run with one-dimensional sensitivity tests for an idealized atmosphere and with data from
Wangara day 33. A simulation over snow cover is also examined. The tests substantiate
the role of vertical mixing in ameliorating nocturnal cooling. An additional improvement is
a more realistic boundary layer height for moderate wind speeds. / Graduation date: 1988
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