Box 1
Contains 30 Results:
1976 Bedload Measurements, East Fork River, Wyoming, 1977
Authors: Luna B. Leopold and William W. Emmett. Abstract: Quantitative measurements of bedload-transport rate in the East Fork River, Wyoming, show large spatial and temporal variabilities in traction load. Originally published: Proceedings of the National Academy of Sciences ; v. 74, no. 7 (July 1977).
Base Level, Aggradation, and Grade, 1979
Techniques and Interpretation: the Sediment Studies of G.K. Gilbert, 1980
The Alexandrian Equation, 1987
Abstract: Discusses the combination of technology, strategy, and leadership in solving hydrologic problems. Originally published: Landa, Edward R., and Simon Ince, eds. The history of hydrology. Washington, D.C.: American Geophysical Union, 1987. (History of Geophysics; v. 3).
Ethos, Equity and the Water Resource, 1990
Abstract: Discusses two concepts from ancient history and their relevance to the field of water in the modern age: 1) democratic governance at the will of the people was effective and responsive as long as there existed an ethos in administration, guiding beliefs even though unwritten into law; 2) democratic guidance was effective when equity-fairness to all-was not submerged to private or narrow interests. The Abel Wolman Distinguished Lecture, February 1990, National Research Council.
Ethos, Equity, and the Water Resource, 1990
"The Abel Wolman 1990 Distinguished Lecture." Originally published: Environment; v. 32, no. 2 (March 1990).
Lag Times for Small Drainage Basins, 1991
Base Level Rise: Gradient of Deposition, 1992
Abstract: A rise in base level, as behind a check dam, causes deposition of sediment. When deposition is complete, the gradient of the deposited surface is only about half that of the original channel. This new gradient does not increase with time. No known method of computation explains how incoming sediment is transported over the low gradient zone of deposition. Originally published: Israel Journal of Earth Sciences; v. 41 (1992).