"OWRR Project No. B-071-COLO.", "Submitted to Office of Water Resources Research, United States Department of the Interior.", "June 1973.", The work upon which this report is based was supported (in part) by funds provided by the United States Department of the Interior, Office of Water Resources Research, as authorized by the Water Resources Research Act of 1964, and pursuant to Grant Agreement No. 14-31-0001-3567.", "AER72-73WRW-RCW-GVS26.", Includes bibliographical references., Mode of access: World Wide Web., PDF version also has name "Colorado Water Resources Research Institute."
"Completion report, OWRR Project No. B-015 COLO", "Submitted to Office of Water Resources Research, U.S. Department of Interior.", "June 30, 1971.", "The work upon which this report is based was supported in part by funds provided by United States Department of the Interior, Office of Water Resources Research, as authorized under the Water Resources Research Act of 1964, Public Law 88-379, Agreement Number 14001-0001-1436 (July 1, 1967 to June 30, 1971), Includes bibliographical references., Electronic version reissued by: Colorado Water Resources Research Institute with updated cover., Mode of access: World Wide Web.
Grant nos. 14-08-001-G895 and 14-08-0001-G1006; project no. 06., "Research ... financed in part by the U.S. Department of the Interior, Geological Survey and Bureau of Reclamation, through the Colorado Water Resources Research Institute in cooperation with the U.S.D.A. Agricultural Research Service.", "June 1987.", Bibliography: p. 21., Mode of access: World Wide Web.
At head of title: Thesis., On cover: June 1987., "Submitted ... in partial fulfillment of the requirements for the Degree of Master of Science, Colorado State University, Fort Collins, Colorado, summer 1987.", Bibliography: p. [76]-80., Mode of access: World Wide Web.
Satellite photographs during the summer months frequently reveal a weather situation in which strong convective development is observed over the Rocky Mountains and several hundred kilometers to the east of the mountains, while the region immediately to the lee is essentially cloud free. It is proposed that an orographically induced mesoscale wave phenomenon may produce this situation., "September 1967.", This report was prepared with support from the National Environmental Satellite Center under grant, Includes bibliographical references (p. 22-23)., Mode of access: World Wide Web.
Two detailed, multi-sensor case studies of mesoscale convective storms occurring in summer over the central and eastern Colorado Rockies are presented., "December, 1979.", Supported by the National Science Foundation under Grant, Supported by the U.S. Bureau of Reclamation, Division of Atmospheric Water Resources under Grant, Supported by the National Aeronautics and Space Administration under Grant, Includes bibliographical references (p. 158-160)., Mode of access: World Wide Web.
The evoluation of low-level flow upstream of the Continental Divide (Rocky Mountains) from being blocked, i.e. unable to surmount the barrier, to becoming unblocked and blocked again is studied observationally and numerically., "March 1993.", This research was supported by the National Science Foundation under grants, Includes bibliographical references (p. 109-113), Mode of access: World Wide Web.
Animations of Next Generation Radar reflectivity images are used to analyze the evolution of convective and stratiform regions of 13 mesoscale convective systems., "Fall 1996.", Includes bibliographical references (p. 78-82)., Mode of access: World Wide Web.
