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  2. Hjulström curve - Wikipedia

    en.wikipedia.org/wiki/Hjulström_curve

    The dimensionless Shields Diagram, in combination with the Shields formula is now unanimously accepted for initiation of sediment motion in rivers. Much work was done on river sediment transport formulae in the second half of the 20th century and that work should be used preferably to Hjulström's curve. [3]

  3. Kawa model - Wikipedia

    en.wikipedia.org/wiki/Kawa_model

    The Kawa model (kawa ), named after the Japanese word for river, is a culturally responsive conceptual framework used in occupational therapy to understand and guide the therapeutic process. [1] Developed by Japanese occupational therapists (OTs), the model draws upon the metaphor of a river to describe human occupation, which according to OTs ...

  4. River morphology - Wikipedia

    en.wikipedia.org/wiki/River_morphology

    The terms river morphology and its synonym stream morphology are used to describe the shapes of river channels 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 ...

  5. River - Wikipedia

    en.wikipedia.org/wiki/River

    A diagram of a possible river with the Strahler number of each tributary labeled. In hydrology , a stream order is a positive integer used to describe the level of river branching in a drainage basin. [ 18 ]

  6. Bradshaw model - Wikipedia

    en.wikipedia.org/wiki/Bradshaw_model

    The Bradshaw Model is an idealised geographical model which suggests how a river's characteristics vary between the upper course and lower course of a river. It indicates how discharge, occupied channel width, channel depth, and average load quantity increase downstream, [1] and other properties such as load particle size, channel bed roughness, and gradient as characteristics that decrease.

  7. Stream power - Wikipedia

    en.wikipedia.org/wiki/Stream_power

    Stream power, originally derived by R. A. Bagnold in the 1960s, is the amount of energy the water in a river or stream is exerting on the sides and bottom of the river. [1] Stream power is the result of multiplying the density of the water, the acceleration of the water due to gravity, the volume of water flowing through the river, and the ...

  8. Today's Wordle Hint, Answer for #1259 on Friday, November 29 ...

    www.aol.com/todays-wordle-hint-answer-1259...

    Today's Wordle Answer for #1259 on Friday, November 29, 2024. Today's Wordle answer on Friday, November 29, 2024, is HIPPO. How'd you do? Next: Catch up on other Wordle answers from this week.

  9. River Continuum Concept - Wikipedia

    en.wikipedia.org/wiki/River_continuum_concept

    River studies that assess riverine biological communities and have determined the species composition of an area can then be compared with the ideal species composition from the River Continuum Concept. From there, any variations in species composition may shed light on disturbances that might be occurring to offset the system.

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