The Rosgen Stream Classification is a system for natural rivers in which morphological arrangements of stream characteristics are organized into relatively homogeneous stream types. This is a widely-used method for classifying streams and rivers based on common patterns of channel morphology.
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- Excerpts of copyrighted material used with permission from Rosgen, D.L. 1996, Applied River Morphology This module introduces the basics of the Rosgen classification system, a widely-used method for classifying streams and rivers based on common patterns of channel morphology.
- Applied river morphology PDF By:David L. Rosgen Published on 1996. This Book was ranked at 36 by Google Books for keyword Applied. Book ID of Applied river morphology's Books is TIHuAAAAMAAJ, Book which was written byDavid L. Rosgenhave ETAG 'XXHRxBdtD8I' Book which was published by since 1996 have ISBNs, ISBN 13 Code is and ISBN 10 Code is.
Adobe photoshop illustrator free trial. The terms river morphology and its synonym stream morphology are used to describe the shapes of riverchannels and how they change in shape and direction over time. The morphology of a river channel is a function of a number of processes and environmental conditions, including the composition and erodibility of the bed and banks (e.g., sand, clay, bedrock); erosion comes from the power and consistency of the current, and can effect the formation of the river's path. Also, vegetation and the rate of plant growth; the availability of sediment; the size and composition of the sediment moving through the channel; the rate of sediment transport through the channel and the rate of deposition on the floodplain, banks, bars, and bed; and regional aggradation or degradation due to subsidence or uplift. River morphology can also be effected by human interaction, which is a way the river responds to a new factor in how the river can change its course. An example of human induced change in river morphology is dam construction, which alters the ebb flow of fluvial water and sediment, therefore creating or shrinking estuarine channels.[1] A river regime is a dynamic equilibrium system, which is a way of classifying rivers into different categories. The four categories of river regimes are Sinuous canali- form rivers, Sinuous point bar rivers, Sinuous braided rivers, and Non-sinuous braided rivers.
Applied River Morphology
The study of river morphology is accomplished in the field of fluvialgeomorphology, the scientific term.
See also[edit]
- Bedload, Suspended load
- Sediment, sedimentation, erosion
- River, Stream, Canal
- Water, Water resource
Rosgen 1994
References[edit]
- ^Bo-yuan Zhu,Yi-tian Li,Yao Yue,Yun-ping Yang. Aggravation of north channels' shrinkage and south channels' development in the Yangtze Estuary under dam-induced runoff discharge flattening. Journal Estuarine, Coastal and Shelf Science. 5 March 2017
- Rosgen, Dave (1996). Applied River Morphology. 2nd ed. (Fort Collins, CO: Wildland Hydrology, publ.) ISBN978-0-9653289-0-6.
- Brice J C. Planform properties of meandering rivers [C].River Meandering, Proceedings of the October 24–26, 1983 Rivers '83 Conference, ASCE. New Orleans, Louisi- ana, 1983. 1-15.
External links[edit]
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