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JOURNAL OF GEOPHYSICAL RESEARCH,
VOL. 111,
F04010,
doi:10.1029/2006JF000490,
2006
Form drag in rivers due to small-scale natural topographic features: 2. Irregular sequences
Jason W. Kean
U.S. Geological Survey, Boulder, Colorado, USA
J. Dungan Smith
U.S. Geological Survey, Boulder, Colorado, USA
Abstract
The size, shape, and spacing of small-scale topographic features found on the boundaries of natural streams, rivers, and floodplains
can be quite variable. Consequently, a procedure for determining the form drag on irregular sequences of different-sized topographic
features is essential for calculating near-boundary flows and sediment transport. A method for carrying out such calculations
is developed in this paper. This method builds on the work of Kean and Smith (2006), which describes the flow field for the
simpler case of a regular sequence of identical topographic features. Both approaches model topographic features as two-dimensional
elements with Gaussian-shaped cross sections defined in terms of three parameters. Field measurements of bank topography are
used to show that (1) the magnitude of these shape parameters can vary greatly between adjacent topographic features and (2)
the variability of these shape parameters follows a lognormal distribution. Simulations using an irregular set of topographic
roughness elements show that the drag on an individual element is primarily controlled by the size and shape of the feature
immediately upstream and that the spatial average of the boundary shear stress over a large set of randomly ordered elements
is relatively insensitive to the sequence of the elements. In addition, a method to transform the topography of irregular
surfaces into an equivalently rough surface of regularly spaced, identical topographic elements also is given. The methods
described in this paper can be used to improve predictions of flow resistance in rivers as well as quantify bank roughness.
Received 20
February
2006;
accepted 14
August
2006;
published 6
December
2006.
Keywords: form drag;
bank roughness;
flow resistance.
Index Terms: 1825 Hydrology: Geomorphology: fluvial (1625); 1815 Hydrology: Erosion; 1856 Hydrology: River channels (0483, 0744); 1842 Hydrology: Irrigation.
Read Full Article (file size: 665595 bytes) Cited by
Citation: Kean, J. W., and J. D. Smith
(2006),
Form drag in rivers due to small-scale natural topographic features: 2. Irregular sequences,
J. Geophys. Res.,
111,
F04010,
doi:10.1029/2006JF000490.
This paper is not subject to U.S. copyright. Published in 2006 by the
American Geophysical Union.
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