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Crowsnest River –4 th order, around 3-4 m 3 /sec—10-20 m wide DA around 400 km2

Fish and other aquatic biota that live in rivers and streams have to contend with the variability of the flow regime. How variable is runoff/discharge? From year to year? From month to month From day to day. Crowsnest River –4 th order, around 3-4 m 3 /sec—10-20 m wide DA around 400 km2.

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Crowsnest River –4 th order, around 3-4 m 3 /sec—10-20 m wide DA around 400 km2

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  1. Fish and other aquatic biota that live in rivers and streams have to contend with the variability of the flow regime. How variable is runoff/discharge? From year to year? From month to month From day to day

  2. Crowsnest River –4th order, around 3-4 m3/sec—10-20 m wide DA around 400 km2

  3. Annual mean discharge of the Crowsnest River at Frank 20 m3/s

  4. Exceedence probability Annual mean discharge of the Crowsnest River at Frank m3/s 0.10 0.25 90 percentile 75 percentile 0.50 50 percentile 25 percentile 10 percentile 0.75 0.90

  5. We can now plot these data on cumulative probability paper Exceedance probability (percentiles) 99.9 99 90 70 50 30 20 10 1 0.1 100 Discharge m3/sec 10.0 o o o o o 1.0 Non-exceedence probability (percentiles) Recurrence interval is the reciprocal of the probability Based on this plot we can estimate that 1 year in 100 there will be a year wetter than 20m3/s and a year drier than 0.8 m3/s, if there is no-longterm climate change

  6. 1 yr out of 4 discharge is above this line Annual average 6.0 m3/s 2 yr out of 4 discharge above this line Annual average 4.1 m3/s 3 yr out of 4 discharge above this line Annual average 2.7 m3/s

  7. Before Ottawa R dams After Ottawa R dams River Management can significantly alter the seasonal hydrograph

  8. St.Lawrence River Flood Plain at Lac St. Pierre—has rarely been flooded since the late fifties—What effect might this have on the river?

  9. The hydrograph Short-term response to a precipitation event How would you expect deforestation to influence this response? ---Consider the terms of the hydrological balance equation

  10. Human activities can markedly influence the shape of the hydrograph • Deforestation • reduces the lag time • raises the peak • reduces the base flow How does deforestation affect the hydrological balance [P-E]DA – DS/Dt Fig 5-2 in your text

  11. We can explain the effects of deforestation on the hydrograph in terms of the hydrological balance, mainly in terms of changes in Evaporation and storage. • Evaporation directly from the soil surface increases when plant cover is reduced, but usually transpiration from plant leaves is decreased more than surface evaporation increases. • leads to increased runoff—more area under the hydrograph curve • Storage is reduced—water stored in plant tissues is removed, and the water holding capacity of soils is reduced by the death of roots. • Thus less of the water from the precipation event goes into recharging storage pools (DS is less), & more water enters the stream directly, reducing the lag time on the rising limb, and giving a higher and sharper peak in the deforested watershed. • Recession will also be faster and base flow lower in the deforested watershed since there will be less storage to sustain the stream flow after the rain stops.

  12. Biological Impacts that generally occur when watersheds are hydrologically disturbed by deforestation • Scouring—increased flashiness of the hydrograph can scour and shift gravels. • Siltation—shortening of hydrological lag time (usually associated with increased overland flow vs percolation--influx of fine particulate matter to streams. • plug up interstitial spaces in gravels & reduce water percolation and oxygen supply to interstitial benthic organisms & fish eggs in the gravels. • Siltation + increased dissolved organic material can reduce light penetration • Nutrient enrichment—hydrological changes usually also increase the influx of Nitrogen & Phosphorus to the stream leading to increased algal growth on the substrate. • Increased temperature &illumination—reduced forest cover, depending on how near to the stream bank trees are cut, can increase light penetration, warming the stream & changing the composition of benthic communities, by reducing survival of cold-water species. • increased illumination can also contribute to increased benthic algal growth on rocks.

  13. Patterns in stream flow and how they generate habitat diversity in streams • Annual discharge patterns—floodplain habitats • Stream meander—pool/riffle alternations • Stream channel changes over time—oxbow lakes, braided streams

  14. Flood plains depend on seasonal variability in river discharge • Flood plain habitats greatly increase biodiversity in river systems. They contribute mostly temporary wetlands, but some remain as permanent because of groundwater inputs. • Important for • Waterfowl, mammals, amphibians, fish, aquatic insects, molluscs etc. • Most of the species found in flood plain wetlands would be lost from the river if the floodplain were not allowed to be flooded regularly.

  15. River flood plains often undergo extensive urban development Oxbow lake and the Chippewa River. Eau Claire, Wisconsin. http://www.uoregon.edu/~millerm/meander.html

  16. Many are also strongly impacted by agriculture

  17. Meander pattern of the Sacramento River, CA, note old abandoned channels and oxbows, and the encroachment of agriculture on the river channel. http://www.uoregon.edu/~millerm/meander.html

  18. Green River, Wyoming Such restoration can involve breaching of levees and removal of dams with the aim of.re-establishing natural floodplain vegetation and habitat http://vernalfishandwildlife.fws.gov/vernalfloodplain.jpg

  19. meanders In streams and rivers of different sizes

  20. Rivers meander when they are traveling on top of a relatively flat surface. • a straight line is not the most efficient path for water to flow. A meandering river will dissipate more energy through friction with the riverbed than one that flows straight • The meander pattern shifts constantly since the river is cutting the bank on the outside of meander loops and depositing alluvial sediment on the inside.

  21. Streams flow down hill and take the path of least resistance, however the path is usually a meandering instead of straight http://www.kented.org.uk/ngfl/rivers/River%20Articles/meander.htm

  22. It takes more velocity to suspend and move larger particles

  23. The erosion that occurs during a flood even may cause the river to take a shortcut from one loop to the next--thus cutoff loop will remain as an oxbow lake. Oxbow lake forming from a river meander

  24. Oxbow lakes and braided channels on the Upper Amazon River http://muller.lbl.gov/travel_photos/AmazonWebPages/AmazonWebPages-Thumbnails/1.jpg

  25. The physical stresses on the river bed during floods often cause a river to change course. The river valley contains many old channels superimposed on each other An important reference on River Meanders Leopold, L.B., and M.G. Wolman, 1960, River Meanders: Geol. Soc. America, Bull., v. 71, pp. 769-794. http://waterknowledge.colostate.edu/meander.htm

  26. Rivers often simultaneously occupy several of their historical channels at once. We call this type of river channel braided A good example of braiding in the river channel

  27. Oldman R Below Summerview Showing old river channels

  28. When rivers cut deeply into the landscape the meander pattern becomes entrenched and from then on shifts downward only. http://courses.missouristate.edu/EMantei/creative/WeathStrem/entrenched.jpg

  29. If you want to learn more about the landforms and deposits created by running water, with particular reference to western Canadian watersheds, take Geography 3035 Fluvial Geomorphology—Hester Jiskoot Other courses of relevence are Geography 4015 Integrated Watershed Management—Jim Byrne And Geography 4012 Hydrology—Stefan Kienzle

  30. Sutcliffe, W.H. 1973 Correlations between seasonal river discharge and landings of American Lobster and Atlantic halibat in the Gulf of St. Lawrence. J.Fish. Res. Bd. Can. 30:856-859.

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