Effects of hydrologic regime on magnitude and frequency of dominant discharge
- 27 March 1976
- journal article
- Published by Elsevier in Journal of Hydrology
- Vol. 29 (1-2) , 51-75
- https://doi.org/10.1016/0022-1694(76)90005-6
Abstract
No abstract availableKeywords
This publication has 11 references indexed in Scilit:
- Effects of high‐magnitude floods on channel form: A case study in Maryland PiedmontWater Resources Research, 1974
- River terrace types in the Coastal Valleys of New South WalesAustralian Geographer, 1972
- Meander geometry arising from varying flowsJournal of Hydrology, 1970
- Channel capacity and the adjustment of streams to hydrologic regimeJournal of Hydrology, 1969
- Definition and Identification of Channel and Overbank Deposits and Their Respective Roles In Flood Plain Formation∗The Professional Geographer, 1967
- A DEFINITION OF DOMINANT DISCHARGEInternational Association of Scientific Hydrology. Bulletin, 1966
- Cross section of a floodplain in a moist region of moderate relief [Pennsylvania]Journal of Sedimentary Research, 1960
- Magnitude and Frequency of Forces in Geomorphic ProcessesThe Journal of Geology, 1960
- Factors Influencing Erosion of a Cohesive River BankAmerican Journal of Science, 1959
- Upper and lower frequency curves for peak rates of runoffEOS, Transactions American Geophysical Union, 1958