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A sorting mechanism for a riffle-pool sequence ; THOMAS LISLE Pacific Southwest Forest and Range Experiment Station, Forest Service, U.S. Department of Agriculture, Berkeley, California. stationed at Arcata.
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www.fs.fed.us/psw/publications/lisle/LisleGSA.pdf
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The objective of this paper is to detail the distribution of mean velocities and turbulence intensities in a forced riffle pool. While limited by the lack of lateral velocity measurements, the data set is of high quality and includes measurements during a bankfull flood.
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www.agu.org/pubs/crossref/2007/2006WR005272.shtml
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In the companion article, we present mean velocity and turbulence intensity statistics at a range of discharges in a forced riffle pool unit and show that the distributions of mean velocity and turbulence are characteristic of nonuniform flows.
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www.agu.org/pubs/crossref/2007/2006WR005274.shtml
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Title;Classification and Analysis of Riffle-Pool Structure. ... The indexes were put to a statistical test for examination of the riffle-pool structure. Since these indexes did not necessarily have normal distribution, a non-parametric test was applied to the examination.
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sciencelinks.jp/j-east/article/200307/000020030703A0162...
sciencelinks.jp/j-east/article/200307/000020030703A0162742.php
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Title: A sorting mechanism for a riffle-pool sequence ... Keywords: PSW4351, stream flows, bed material, sorting mechanism, riffle-pool ... Lisle, Thomas 1979. A sorting mechanism for a riffle-pool sequence. Geological Society of America Bulletin, Vol. 90. Part II, p. 1142-1157.
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www.treesearch.fs.fed.us/pubs/7832
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Keywords: PSW4351, aggradaton, degradation, stream channel, geomorphic, riffle-pool morphology, California, sediment load, hillslope, erosion ... Lisle, Thomas E. 1982. Effects of aggradation and degradation on riffle-pool morphology in natural gravel channels, northwestern California. Water Resources Research 18(6):
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www.treesearch.fs.fed.us/pubs/7843
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Longitudinal profile and floodplain data of a low-gradient, riffle-pool stream near Stockton, MN, were collected using a laser-prism total station, and channel velocity profiles and discharge were measured using an Acoustic Doppler Velocimeter.
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gsa.confex.com/gsa/2007SC/finalprogram/abstract_119964....
gsa.confex.com/gsa/2007SC/finalprogram/abstract_119964.htm
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Investigations of channel geometry in a headwater stream in Cornwall, England, reveal that systematic variations of channel width occur in conjunction with the oscillations of bed topography in the riffle-pool sequence.
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bulletin.geoscienceworld.org/cgi/content/abstract/87/6/...
bulletin.geoscienceworld.org/cgi/content/abstract/87/6/883
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Despite the occurrence of pool-riffle sequences in many rivers there are few data concerning pool-riffle unit morphology. Of many criteria proposed to identify pool-riffle units, only two methods can be regarded as objective and robust. ... typically H ï 0.16h. Riffle height is a positive function of riffle length.
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