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 –4th order, around 3-4 m3/sec—10-20 m wide DA around 400 km2
Annual mean discharge of the Crowsnest River at Frank
20
m3/s
14
12
10
8
6
4
2
0
1982
1987
1992
1997
2002
2007
Exceedence probability
Annual mean discharge of the Crowsnest River at Frank
0.10
0.25
0.50
0.75
0.90
1995
12
1991
9.8
2005
8.7
1993
6.3
2002
6.2
1996
5.9
1992
5.5
2004
4.6
1999
4.4
1994
4.2
1986
4.1
1990
3.8
1988
3.7
1989
3.5
1998
3.1
1987
2.5
1997
1.7
2003
1.5
2000
1.4
2001
1.2
m3/s
14
12
10
90 percentile
8
6
75 percentile
4
50 percentile
2
25 percentile
10 percentile
0
1982
1987
1992
1997
2002
2007
We can now plot these data on cumulative probability paper
Exceedance probability (percentiles)
99.9 99
90
70
50
30 20 10
1
o
0.1
100
10.0
Discharge
m3/sec
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
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
Before Ottawa R dams
After Ottawa R dams
River Management can significantly
alter the seasonal hydrograph
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?
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
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
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.
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.
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
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.
River flood plains often undergo extensive urban development
Oxbow lake and the Chippewa River. Eau Claire, Wisconsin.
http://www.uoregon.edu/~millerm/meander.html
Many are also strongly impacted by agriculture
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
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
meanders
In streams and rivers of
different sizes
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.
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
It takes more
velocity to suspend
and move larger
particles
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
Oxbow lakes and braided channels on the Upper Amazon River
http://muller.lbl.gov/travel_photos/AmazonWebPages/AmazonWebPages-Thumbnails/1.jpg
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
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
Oldman R
Below
Summerview
Showing old
river
channels
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
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
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.