"Research Supported by Department of Defense Center for Geosciences/Atmospheric Research (CG/AR), under cooperative agreement #DAAD-19-02-2-2005.", "1 November 2005.", "DoD Center for Geosciences/Atmospheric Research under grant DAAD19-02-2-0005."--Cover., Includes bibliographical references., Mode of access: World Wide Web.
"April 1970.", This study has been supported by the National Science Foundation under NSF Grant GA-12980 NSF Grant GA-12980.", Includes bibliographical references (p. 44-45)., Mode of access: World Wide Web.
edited by Robert E. Moreng., Summarizes the results of research undertaken by the Western Regional Technical Committee W-142., Includes bibliographical references., Print version record.
Wind-tunnel transient concentration data were obtained from modeling tests which reproduced gaseous dispersion from five different forty cubic meter or less liquefied natural gas (LNG) spills performed at China Lake Naval Weapons Center. Comparisons in the transient concentration data between these modeled tests and the field tests indicated which parameters are dominant in the modeling process. Model tests which reproduced the wind shear and turbulence structure of the approach wind reproduced the concentration patterns measured at the field site. This result reinforced the predictive reliability of wind tunnel modeling of larger volume spills., prepared by D.E. Neff and R.N. Meroney., "CER81-82DEN-RNM1.", "July 1981.", Includes bibliographical references., "For Gas Research Institute, contract no. 5014-352-0203.", Print version record.
Visual and concentration measurements were made for a large number of continuous ground-level releases of heavy gases into a wind-tunnel boundary layer. These different plumes were not affected by any topographic or building wake influences. The experiments provided a broad coverage of the variable range of source gas specific gravity, source gas flow rate, and approach flow wind speed., prepared by D.E. Neff and R.N. Meroney., "CER81-82DEN-RNM25.", "March 1982.", Includes bibliographical references., Gas Research Institute, contract no. 5014-352-0203., Print version record.
Cover title., "May 1900.", "Technical series no. 5"--Cover., Pagination is a continuation of Bulletins 37 and 44., Includes bibliographical references (p. 186-189) and index., Mode of access: World Wide Web.
[prepared February 26, 1943 by H.S. Wilgus, Jr., R.C. Tom, and L.E. Washburn]., "Misc. series 190" handwritten on first page., Typescript., "(7219)-43"--Leaf 3., Caption title., Print version record.
As a young boy, William (Willie) Wilson Curtin was on the dignities platform when the Gettysburg cemetery was consecrated. A photograph shows Abraham Lincoln and Willie Curtin, son of Pennsylvania's Governor Andrew Curtin just prior to Lincoln giving the famed Gettysburg address. The history of Gettysburg battle and cemetery and the impact of the Gettysburg address are discussed., video file MPEG 536MB, Executive producer: Roger Sharpe; written by Joe Vasos and Roger Sharpe; directed by Joe Vasos; narrated by Rosemary Harris; graphics Joe Mendoza, Carl Kichinko; original music composed and performed by Katherine Azari., "The Boy Who Heard Lincoln at Gettysburg was inspired by the historical research of Roger Sharpe.", Produced by Colorado State University., Online resource; title from title screen (viewed February 2020)
A study of ozone chemistry and meteorological processes occurring in the eastern North Pacific stratocumulus regime. This climatological regime is characterized by widespread, persistent low cloud and an air history that does not include contact with continents for many days. Since both ozone and important in the earth-atmosphere energy balance, the processes studied here are important in the system interactions that govern climate., "Research supported by the National Science Foundation, "Research supported by the National Science Foundation, "Research supported by the National Science Foundation, "September, 1988.", Includes bibliographical references (p. [82]-91)., Mode of access: World Wide Web.