Bankfull Regional Curves for Streams in the Non-Urban, Non-Tidal Coastal Plain Physiographic Province, Virginia and Maryland
暂无分享，去创建一个
[1] Luna Bergere Leopold,et al. The View from the River: , 1994 .
[2] G. Pickup,et al. Effects of hydrologic regime on magnitude and frequency of dominant discharge , 1976 .
[3] M. Gordon Wolman,et al. Fluvial Processes in Geomorphology , 1965 .
[4] G. Williams. Bank‐full discharge of rivers , 1978 .
[5] M. Wolman,et al. Magnitude and Frequency of Forces in Geomorphic Processes , 1960, The Journal of Geology.
[6] E. Andrews. Effective and bankfull discharges of streams in the Yampa River basin, Colorado and Wyoming , 1980 .
[7] A. Ernst,et al. Regionalized equations for bankfull-discharge and channel characteristics of streams in New York state: hydrologic region 5 in central New York , 2005 .
[8] Keith Richards,et al. Rivers: Form and Process in Alluvial Channels , 1982 .
[9] L. B. Leopold,et al. Water In Environmental Planning , 1978 .
[10] D. Rosgen. A classification of natural rivers , 1994 .
[11] Jeffrey J. Chaplin. Development of regional curves relating bankfull-channel geometry and discharge to drainage area for streams in Pennsylvania and selected areas of Maryland , 2005 .
[12] M. Wolman. A method of sampling coarse river‐bed material , 1954 .
[13] Cheryl C Harrelson,et al. Stream Channel Reference Sites: An Illustrated Guide to Field Technique , 1994 .
[14] James M. Sherwood,et al. Bankfull characteristics of Ohio streams and their relation to peak streamflows , 2005 .