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Characterizing change of high frequency
return periods in urbanizing southern
Ontario watersheds
Peter John Thompson
Earthfx Inc.
Dr. William K. Annable
Department of Civil and Environmental Engineering
University of Waterloo
CWRA 2014 Canada Water Resources Congress
June 2, 2014
Effects of
Urbanization
• Increase in impervious area
• Shorter events
• Larger peak discharge
• Infiltration
• Changes to frequency
• Channelization
• Change in vegetative cover
• Habitat degradation
• Erosion
• Poor water quality
• Failure of engineered structures
2
3
Environment Canada
(Water Survey Division)
Gauged Catchments
Study Catchments
Environment Canada
(Water Survey Division)
Gauged CatchmentsStudy Catchments
5
Middle Don River, North York c. 1954-55
Aerial Photographic Analysis
Highway 401
under
construction
RCAF Station
Downsview
Aerial Photographic Analysis
6
Don River at York Mills c. 1955
• Scanned and
georeferenced aerial
photographs in 8-year
intervals from 1954 to
2010
• Identified urbanized
areas by hand
Aerial Photographic Analysis
7
Don River at York Mills c. 2005
• Two temporal datasets
produced:
• “Effective Impervious
Area” (EIA)
• Road Density
• Can we relate this
observed change to
hydrologic variables?
Little Don River
at Don Mills
(02HC029)
1954
Don River at York
Mills
(02HC005)
0 2 4 6 8 101
Kilometers
Effective Catchment Area
Road Network - 1954
Forested Cover - 1955
Urbanized Area - 1954
1960
Don River at York
Mills
(02HC005)
Little Don River
at Don Mills
(02HC029)
0 2 4 6 8 101
Kilometers
Effective Catchment Area
Road Network - 1960
Urbanized Area - 1960
1970
Don River at York
Mills
(02HC005)
Little Don River
at Don Mills
(02HC029)
0 2 4 6 8 101
Kilometers
Effective Catchment Area
Road Network - 1970
Urbanized Area - 1970
1978
Don River at York
Mills
(02HC005)
Little Don River
at Don Mills
(02HC029)
0 2 4 6 8 101
Kilometers
Effective Catchment Area
Road Network - 1978
Urbanized Area - 1978
1995
Don River at York
Mills
(02HC005)
Little Don River
at Don Mills
(02HC029)
2005
Don River at York
Mills
(02HC005)
Little Don River
at Don Mills
(02HC029)
Land Use Change
Transition from Agricultural to Urban Land Use
0
2
4
6
8
10
12
0
10
20
30
40
50
60
70
80
90
100
1950 1960 1970 1980 1990 2000 2010
RoadDensity(km/km2)
PercentArea
Year
Urbanized Area
Agricultural Area
Catchment Road Density
02HC005 – Don River at York Mills
Effective Catchment Area – 95.5 km2
Etobicoke Creek below QEW (02HC030)
1970
• Effective Catchment Area - 204 km2
• Urbanized Area - 45.4 km2 (21%)
• Total Road Length - 718 km
0 4 8 122
Kilometers
Effective Catchment Area
Road Network - 1970
Urbanized Area - 1970
Etobicoke Creek below QEW (02HC030)
1978
• Effective Catchment Area - 204 km2
• Urbanized Area - 64.2 km2 (30%)
• Total Road Length - 908 km
0 4 8 122
Kilometers
Effective Catchment Area
Road Network - 1978
Urbanized Area - 1978
Etobicoke Creek below QEW (02HC030)
1995
• Effective Catchment Area - 204 km2
• Urbanized Area - 100 km2 (47%)
• Total Road Length - 1380 km
0 4 8 122
Kilometers
Effective Catchment Area
Road Network - 1995
Urbanized Area - 1995
Etobicoke Creek below QEW (02HC030)
2005
• Effective Catchment Area - 204 km2
• Urbanized Area - 54.9 km2 (55%)
• Total Road Length - 1540 km
0 4 8 122
Kilometers
Effective Catchment Area
Road Network - 2005
Urbanized Area - 2005
Temporal Land Use Change
Redhill Creek at Hamilton (02HA014)
20
• Effective Catchment Area
57.0 km2
• Urbanized Area
~60%
AAfafdas
Hydrograph Change with Urbanization
Time (T) Time (T)
Rainfall(L)
Discharge(L3/T)
After
Urbanization
Original
Lag time after
urbanization
Hydrograph
of streamflow
Lag time
Center of mass
of runoff
and of rainfall
Discharge(L3/T)
Rainfall
•Changes to event hydrograph with urbanization...?
after Leopold (1968)
Daily vs. Instantaneous Data
22
02HA014 – Redhill Creek at Hamilton
• The daily stream
flow represents an
average, the
instantaneous data
is made up of 15
minute interval
measurements
• Individual events
and event peaks
can be clearly
identified on the 15
minute hydrograph
Instantaneous Stream Flow Data
Manual Chart Digitizing (c. ~1975)
• Need high resolution, high frequency data
• Only data available post-1996
• Joint project with Water Survey of Canada
• Archived electronic records dating from 1969 were
processed to create a
15 minute resolution
hydrograph
• Much of this data was
originally digitized by
hand
Daily vs. Instantaneous Data
• Periods of high flow are not captured on the
mean daily hydrograph 24
02HC029 – Little Don River at Don Mills
Event Separation Algorithm
25
• Allows individual
events to be parsed
and analyzed from
the instantaneous
hydrometric record
• Events are
considered over
after the Q passes
below some ratio of
the peak
• Thresholds range
from 15% - 50% of
peak discharge02HA014 - Redhill Creek at Hamilton
26
Event Separation Algorithm
• Most events during
the year can be
identified
• There is no
instantaneous record
for backwater periods
due to ice or
vegetation
• Data lends itself to
urban catchments or
analysis of warm
weather events
(May – November)
02HA014 - Redhill Creek at Hamilton
BackwaterDuetoIce
Event Separation Algorithm
27
02HC033 - Mimico Creek at Islington
BackwaterDuetoIce
Mann-Kendall Trend (5% CI): Increasing
Peak Event Discharge
Station Name Trend
Duffins Creek above Pickering
East Humber River near Pine Grove
East Oakville Creek near Omagh
Laurel Creek at Waterloo ↑
Redhill Creek at Hamilton
Black Creek near Weston ↑
Etobicoke Creek at Brampton ↑
Etobicoke Creek below QEW ↑
Mimico Creek at Islington ↑
Don River at York Mills ↑
Little Don River at Don Mills ↑
Don River at Todmorden ↑
Rouge River near Markham ↑
Highland Creek near West Hill ↑
Harmony Creek at Oshawa ↑
Peak Event Discharge
UrbanizedRural
Frequency Analysis
• Can we relate changes in the urban footprint
to changes in return frequency?
• Need to assess hydrologic change in step with
catchment land use change
30
Land Use Change
31
Highland Creek near West Hill
(02HC013)
Urban Area
Road Density
Space for Time Substitution
32
Highland Creek near West Hill
(02HC013)
(Peak Discharge)
Space for Time Substitution
33
(Peak Discharge)
Highland Creek near West Hill
(02HC013)
34
Highland Creek near West Hill
(02HC013)
Moving Window Weibull Recurrence Interval =
Length of Record + 1
Event Rank
35
Little Don River at Don Mills
(02HC029)
Return Frequency
(7-Year Moving Weibull Plot)
Return Frequency
(7-Year Moving Weibull Plot)
36
Highland Creek near West Hill
(02HC013)
37
Don River at Todmorden
(02HC024)
Return Frequency
(7-Year Moving Weibull Plot)
38
Rouge River near Markham
(02HC022)
Return Frequency
(7-Year Moving Weibull Plot)
Conclusions
• Event based separation allows high resolution datasets to be
parsed down to hydrological descriptive variables
• The magnitude of change in storm peaks varies with return
frequency, but these changes may not be consistent
• Spatial distribution of build-out critical to understanding
hydrologic change
• These data can be used for Partial Peak, and Partial Duration,
and Annual Duration methods to fine tune the analysis of
higher frequency events in urban catchments
A Nonstationary Analysis of Southern Ontario Storm Events
Identified from High Resolution Streamflow Data;
Nicole L. O’Brien, Peter J. Thompson, Donald H. Burn,
William K. Annable
Session M2C
Acknowledgements
Dr. Herman Goertz Jeanette Fooks
Paula Hunter Carrie-Lynn Green
Water Survey Division, Environment Canada
Tom Arsenault
Aerial Photography Analysis Eco-Hydraulics Co-op
Robert Leonard Tyler Gale
Nikita Tirskikh Victoria Lounder
Chris McKie Ben Plumb
Christina Bright
CompuMOD Dataset Extraction
Ian McLaurin
41
Thank you!
Questions or
Comments?
WSC
Station ID
Station Name
Area
(km2)
Percent
Urban
(1969)
Percent
Urban
(≈2010)
Percent
Change
02HC019 Duffins Creek above Pickering 93.5 > 5% --
02HC009 East Humber River near Pine Grove 197 > 10% --
02HB004 East Oakville Creek near Omagh 199 > 10% --
02GA024 Laurel Creek at Waterloo 57.5 15 38 23
02HA014 Red Hill Creek at Hamilton 57.0 27 60 33
02HC027 Black Creek near Weston 66.0 55 78 22
02HC017 Etobicoke Creek at Brampton 65.1 1 18 17
02HC030 Etobicoke Creek below QEW 211 20 55 34
02HC033 Mimico Creek at Islington 75.2 43 82 39
02HC005 Don River at York Mills 96.7 30 69 39
02HC029 Little Don River at Don Mills 138 30 68 38
02HC024 Don River at Todmorden 321 43 73 30
02HC022 Rouge River near Markham 181 7 40 33
02HC013 Highland Creek near West Hill 89.0 47 86 39
02HD013 Harmony Creek at Oshawa 42.1 20 45 25
42
Study Catchments
Mann-Kendall Test
• Non-parametric test for monotonic trends
• Independent events assumed to be
uncorrelated
• Trends tested to a 95% significance level
( p ≤ 0.025 )
 









0if1
0if0
0if1
sgn



  

 

1
1 1
sgn
n
k
n
kj
kj xxS
43
Typical Event Hydrograph
44
Qpeak
Qthreshold
Qstart
Qend
Time
Discharge
tstart tpeak tthreshold
Trise Tthreshold Ttotal
Vrise
Q75
Q50
T75
T50
Rising
Limb
Falling
Limb
Recession
Limb
Vrecession
Vtotal
tend
• Once an event has be
identified on the
hydrograph, specific
event properties can
be analyzed
• Event volume,
duration, time to
peak, etc. can be
calculated directly
from the observed
hydrograph
• Trends in event
parameters can be
explored
Peak Event Discharge
Station Name Trend
Duffins Creek above Pickering
East Humber River near Pine Grove
East Oakville Creek near Omagh
Laurel Creek at Waterloo ↑
Redhill Creek at Hamilton
Black Creek near Weston ↑
Etobicoke Creek at Brampton ↑
Etobicoke Creek below QEW ↑
Mimico Creek at Islington ↑
Don River at York Mills ↑
Little Don River at Don Mills ↑
Don River at Todmorden ↑
Rouge River near Markham ↑
Highland Creek near West Hill ↑
Harmony Creek at Oshawa ↑
Number of Events per Year
Station Name Trend
Duffins Creek above Pickering
East Humber River near Pine Grove
East Oakville Creek near Omagh
Laurel Creek at Waterloo
Redhill Creek at Hamilton
Black Creek near Weston
Etobicoke Creek at Brampton ↑
Etobicoke Creek below QEW
Mimico Creek at Islington
Don River at York Mills ↑
Little Don River at Don Mills ↑
Don River at Todmorden
Rouge River near Markham ↑
Highland Creek near West Hill ↑
Harmony Creek at Oshawa ↑
Event Volume
Station Name Trend
Duffins Creek above Pickering
East Humber River near Pine Grove
East Oakville Creek near Omagh
Laurel Creek at Waterloo ↑
Redhill Creek at Hamilton ↑
Black Creek near Weston
Etobicoke Creek at Brampton ↑
Etobicoke Creek below QEW ↑
Mimico Creek at Islington ↑
Don River at York Mills ↓
Little Don River at Don Mills ↑
Don River at Todmorden ↑
Rouge River near Markham ↑
Highland Creek near West Hill
Harmony Creek at Oshawa
Total Event Duration
Station Name Trend
Duffins Creek above Pickering
East Humber River near Pine Grove
East Oakville Creek near Omagh ↓
Laurel Creek at Waterloo
Redhill Creek at Hamilton
Black Creek near Weston ↓
Etobicoke Creek at Brampton ↓
Etobicoke Creek below QEW ↑
Mimico Creek at Islington ↑
Don River at York Mills ↓
Little Don River at Don Mills ↑
Don River at Todmorden ↓
Rouge River near Markham ↑
Highland Creek near West Hill ↓
Harmony Creek at Oshawa ↓
Event Quick Flow
(Direct Runoff) Volume
Station Name Trend
Duffins Creek above Pickering
East Humber River near Pine Grove
East Oakville Creek near Omagh
Oakville Creek at Milton ↓
Credit River near Orangeville
Black Creek near Weston
Etobicoke Creek at Brampton ↑
Etobicoke Creek below QEW ↑
Mimico Creek at Islington ↑
Don River at York Mills
Little Don River at Don Mills ↑
Don River at Todmorden
Rouge River near Markham ↑
Highland Creek near West Hill ↑
Harmony Creek at Oshawa
MK Trend: Increasing
Event Interflow Volume
Station Name Trend
Duffins Creek above Pickering ↑
East Humber River near Pine Grove
East Oakville Creek near Omagh
Oakville Creek at Milton
Credit River near Orangeville
Black Creek near Weston ↑
Etobicoke Creek at Brampton
Etobicoke Creek below QEW ↑
Mimico Creek at Islington ↑
Don River at York Mills
Little Don River at Don Mills ↑
Don River at Todmorden ↑
Rouge River near Markham ↑
Highland Creek near West Hill ↑
Harmony Creek at Oshawa ↑
MK Trend: Increasing
Station Name
Peak
Discharg
e
Time
to
Peak
Event
Duration
Total
Hydrograp
h Duration
Event
Volume
Total
Hydrograp
h Volume
Flashines
s
Duffins Creek above Pickering
East Humber River near Pine Grove
East Oakville Creek near Omagh ↓
Oakville Creek at Milton ↑ ↓ ↓ ↓ ↓ ↓ ↑
Credit River near Orangeville ↑
Laurel Creek at Waterloo ↑ ↑ ↑ ↑ ↑
Redhill Creek at Hamilton ↑
Black Creek near Weston ↑ ↓ ↑
Etobicoke Creek at Brampton ↑ ↓ ↓ ↓ ↑ ↑ ↑
Etobicoke Creek below QEW ↑ ↑ ↑ ↑ ↑ ↑
Mimico Creek at Islington ↑ ↑ ↑ ↑ ↑ ↑
Don River at York Mills ↑ ↓ ↓ ↓ ↓ ↑
Little Don River at Don Mills ↑ ↑ ↑ ↑ ↑ ↑ ↑
Don River at Todmorden ↑ ↓ ↓ ↑ ↑ ↑
Rouge River near Markham ↑ ↑ ↑ ↑ ↑ ↑
Highland Creek near West Hill ↑ ↓ ↓ ↓ ↑ ↑
Harmony Creek at Oshawa ↑ ↓ ↓ ↑
Summary (Warm Weather Trends)
Mimico Creek at Islington (02HC033)
1970
• Effective Catchment Area - 215 km2
• Urbanized Area - 33.3 km2 (45%)
• Total Road Length - 450 km
0 2 4 61
Kilometers
Effective Catchment Area
Road Network - 1970
Urbanized Area - 1970
Mimico Creek at Islington (02HC033)
1978
• Effective Catchment Area - 215 km2
• Urbanized Area - 40.2 km2 (55%)
• Total Road Length - 553 km
0 2 4 61
Kilometers
Effective Catchment Area
Road Network - 1978
Urbanized Area - 1978
Mimico Creek at Islington (02HC033)
1995
• Effective Catchment Area - 215 km2
• Urbanized Area – 53.0 km2 (72%)
• Total Road Length - 641 km
0 2 4 61
Kilometers
Effective Catchment Area
Road Network - 1995
Urbanized Area - 1995
Mimico Creek at Islington (02HC033)
2005
• Effective Catchment Area - 215 km2
• Urbanized Area - 60.2 km2 (81.5%)
• Total Road Length - 683 km
0 2 4 61
Kilometers
Road Network - 2005
Effective Catchment Area
Urbanized Area - 2005
Highland Creek near West Hill
(02HC013)
1955
• Effective Catchment Area - 89 km2
• Urbanized Area - 8.9 km2 (10%)
• Total Road Length - 248 km
0 1 2 3 40.5
Kilometers
Topographic Catchment Boundary
Road Network - 1955
Forest Cover - 1955
Urbanized Area - 1955
Highland Creek near West Hill
(02HC013)
2010
• Effective Catchment Area - 89 km2
• Urbanized Area - 76.5 km2 (86%)
• Total Road Length - 876 km
0 1 2 3 40.5
Kilometers
Topographic Catchment Boundary
Road Network - 2010
Urbanized Area - 2010
Change in 1.5 Year Return Discharge
58
Change in Bankfull Discharge
59

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Characterizing Change of High Frequency Return Periods in Urbanizing Southern Ontario Watersheds

  • 1. Characterizing change of high frequency return periods in urbanizing southern Ontario watersheds Peter John Thompson Earthfx Inc. Dr. William K. Annable Department of Civil and Environmental Engineering University of Waterloo CWRA 2014 Canada Water Resources Congress June 2, 2014
  • 2. Effects of Urbanization • Increase in impervious area • Shorter events • Larger peak discharge • Infiltration • Changes to frequency • Channelization • Change in vegetative cover • Habitat degradation • Erosion • Poor water quality • Failure of engineered structures 2
  • 3. 3 Environment Canada (Water Survey Division) Gauged Catchments Study Catchments
  • 4. Environment Canada (Water Survey Division) Gauged CatchmentsStudy Catchments
  • 5. 5 Middle Don River, North York c. 1954-55 Aerial Photographic Analysis Highway 401 under construction RCAF Station Downsview
  • 6. Aerial Photographic Analysis 6 Don River at York Mills c. 1955 • Scanned and georeferenced aerial photographs in 8-year intervals from 1954 to 2010 • Identified urbanized areas by hand
  • 7. Aerial Photographic Analysis 7 Don River at York Mills c. 2005 • Two temporal datasets produced: • “Effective Impervious Area” (EIA) • Road Density • Can we relate this observed change to hydrologic variables?
  • 8. Little Don River at Don Mills (02HC029) 1954 Don River at York Mills (02HC005) 0 2 4 6 8 101 Kilometers Effective Catchment Area Road Network - 1954 Forested Cover - 1955 Urbanized Area - 1954
  • 9. 1960 Don River at York Mills (02HC005) Little Don River at Don Mills (02HC029) 0 2 4 6 8 101 Kilometers Effective Catchment Area Road Network - 1960 Urbanized Area - 1960
  • 10. 1970 Don River at York Mills (02HC005) Little Don River at Don Mills (02HC029) 0 2 4 6 8 101 Kilometers Effective Catchment Area Road Network - 1970 Urbanized Area - 1970
  • 11. 1978 Don River at York Mills (02HC005) Little Don River at Don Mills (02HC029) 0 2 4 6 8 101 Kilometers Effective Catchment Area Road Network - 1978 Urbanized Area - 1978
  • 12. 1995 Don River at York Mills (02HC005) Little Don River at Don Mills (02HC029)
  • 13. 2005 Don River at York Mills (02HC005) Little Don River at Don Mills (02HC029)
  • 14. Land Use Change Transition from Agricultural to Urban Land Use 0 2 4 6 8 10 12 0 10 20 30 40 50 60 70 80 90 100 1950 1960 1970 1980 1990 2000 2010 RoadDensity(km/km2) PercentArea Year Urbanized Area Agricultural Area Catchment Road Density 02HC005 – Don River at York Mills Effective Catchment Area – 95.5 km2
  • 15. Etobicoke Creek below QEW (02HC030) 1970 • Effective Catchment Area - 204 km2 • Urbanized Area - 45.4 km2 (21%) • Total Road Length - 718 km 0 4 8 122 Kilometers Effective Catchment Area Road Network - 1970 Urbanized Area - 1970
  • 16. Etobicoke Creek below QEW (02HC030) 1978 • Effective Catchment Area - 204 km2 • Urbanized Area - 64.2 km2 (30%) • Total Road Length - 908 km 0 4 8 122 Kilometers Effective Catchment Area Road Network - 1978 Urbanized Area - 1978
  • 17. Etobicoke Creek below QEW (02HC030) 1995 • Effective Catchment Area - 204 km2 • Urbanized Area - 100 km2 (47%) • Total Road Length - 1380 km 0 4 8 122 Kilometers Effective Catchment Area Road Network - 1995 Urbanized Area - 1995
  • 18. Etobicoke Creek below QEW (02HC030) 2005 • Effective Catchment Area - 204 km2 • Urbanized Area - 54.9 km2 (55%) • Total Road Length - 1540 km 0 4 8 122 Kilometers Effective Catchment Area Road Network - 2005 Urbanized Area - 2005
  • 20. Redhill Creek at Hamilton (02HA014) 20 • Effective Catchment Area 57.0 km2 • Urbanized Area ~60%
  • 21. AAfafdas Hydrograph Change with Urbanization Time (T) Time (T) Rainfall(L) Discharge(L3/T) After Urbanization Original Lag time after urbanization Hydrograph of streamflow Lag time Center of mass of runoff and of rainfall Discharge(L3/T) Rainfall •Changes to event hydrograph with urbanization...? after Leopold (1968)
  • 22. Daily vs. Instantaneous Data 22 02HA014 – Redhill Creek at Hamilton • The daily stream flow represents an average, the instantaneous data is made up of 15 minute interval measurements • Individual events and event peaks can be clearly identified on the 15 minute hydrograph
  • 23. Instantaneous Stream Flow Data Manual Chart Digitizing (c. ~1975) • Need high resolution, high frequency data • Only data available post-1996 • Joint project with Water Survey of Canada • Archived electronic records dating from 1969 were processed to create a 15 minute resolution hydrograph • Much of this data was originally digitized by hand
  • 24. Daily vs. Instantaneous Data • Periods of high flow are not captured on the mean daily hydrograph 24 02HC029 – Little Don River at Don Mills
  • 25. Event Separation Algorithm 25 • Allows individual events to be parsed and analyzed from the instantaneous hydrometric record • Events are considered over after the Q passes below some ratio of the peak • Thresholds range from 15% - 50% of peak discharge02HA014 - Redhill Creek at Hamilton
  • 26. 26 Event Separation Algorithm • Most events during the year can be identified • There is no instantaneous record for backwater periods due to ice or vegetation • Data lends itself to urban catchments or analysis of warm weather events (May – November) 02HA014 - Redhill Creek at Hamilton BackwaterDuetoIce
  • 27. Event Separation Algorithm 27 02HC033 - Mimico Creek at Islington BackwaterDuetoIce
  • 28. Mann-Kendall Trend (5% CI): Increasing Peak Event Discharge
  • 29. Station Name Trend Duffins Creek above Pickering East Humber River near Pine Grove East Oakville Creek near Omagh Laurel Creek at Waterloo ↑ Redhill Creek at Hamilton Black Creek near Weston ↑ Etobicoke Creek at Brampton ↑ Etobicoke Creek below QEW ↑ Mimico Creek at Islington ↑ Don River at York Mills ↑ Little Don River at Don Mills ↑ Don River at Todmorden ↑ Rouge River near Markham ↑ Highland Creek near West Hill ↑ Harmony Creek at Oshawa ↑ Peak Event Discharge UrbanizedRural
  • 30. Frequency Analysis • Can we relate changes in the urban footprint to changes in return frequency? • Need to assess hydrologic change in step with catchment land use change 30
  • 31. Land Use Change 31 Highland Creek near West Hill (02HC013) Urban Area Road Density
  • 32. Space for Time Substitution 32 Highland Creek near West Hill (02HC013) (Peak Discharge)
  • 33. Space for Time Substitution 33 (Peak Discharge) Highland Creek near West Hill (02HC013)
  • 34. 34 Highland Creek near West Hill (02HC013) Moving Window Weibull Recurrence Interval = Length of Record + 1 Event Rank
  • 35. 35 Little Don River at Don Mills (02HC029) Return Frequency (7-Year Moving Weibull Plot)
  • 36. Return Frequency (7-Year Moving Weibull Plot) 36 Highland Creek near West Hill (02HC013)
  • 37. 37 Don River at Todmorden (02HC024) Return Frequency (7-Year Moving Weibull Plot)
  • 38. 38 Rouge River near Markham (02HC022) Return Frequency (7-Year Moving Weibull Plot)
  • 39. Conclusions • Event based separation allows high resolution datasets to be parsed down to hydrological descriptive variables • The magnitude of change in storm peaks varies with return frequency, but these changes may not be consistent • Spatial distribution of build-out critical to understanding hydrologic change • These data can be used for Partial Peak, and Partial Duration, and Annual Duration methods to fine tune the analysis of higher frequency events in urban catchments A Nonstationary Analysis of Southern Ontario Storm Events Identified from High Resolution Streamflow Data; Nicole L. O’Brien, Peter J. Thompson, Donald H. Burn, William K. Annable Session M2C
  • 40. Acknowledgements Dr. Herman Goertz Jeanette Fooks Paula Hunter Carrie-Lynn Green Water Survey Division, Environment Canada Tom Arsenault Aerial Photography Analysis Eco-Hydraulics Co-op Robert Leonard Tyler Gale Nikita Tirskikh Victoria Lounder Chris McKie Ben Plumb Christina Bright CompuMOD Dataset Extraction Ian McLaurin
  • 42. WSC Station ID Station Name Area (km2) Percent Urban (1969) Percent Urban (≈2010) Percent Change 02HC019 Duffins Creek above Pickering 93.5 > 5% -- 02HC009 East Humber River near Pine Grove 197 > 10% -- 02HB004 East Oakville Creek near Omagh 199 > 10% -- 02GA024 Laurel Creek at Waterloo 57.5 15 38 23 02HA014 Red Hill Creek at Hamilton 57.0 27 60 33 02HC027 Black Creek near Weston 66.0 55 78 22 02HC017 Etobicoke Creek at Brampton 65.1 1 18 17 02HC030 Etobicoke Creek below QEW 211 20 55 34 02HC033 Mimico Creek at Islington 75.2 43 82 39 02HC005 Don River at York Mills 96.7 30 69 39 02HC029 Little Don River at Don Mills 138 30 68 38 02HC024 Don River at Todmorden 321 43 73 30 02HC022 Rouge River near Markham 181 7 40 33 02HC013 Highland Creek near West Hill 89.0 47 86 39 02HD013 Harmony Creek at Oshawa 42.1 20 45 25 42 Study Catchments
  • 43. Mann-Kendall Test • Non-parametric test for monotonic trends • Independent events assumed to be uncorrelated • Trends tested to a 95% significance level ( p ≤ 0.025 )            0if1 0if0 0if1 sgn           1 1 1 sgn n k n kj kj xxS 43
  • 44. Typical Event Hydrograph 44 Qpeak Qthreshold Qstart Qend Time Discharge tstart tpeak tthreshold Trise Tthreshold Ttotal Vrise Q75 Q50 T75 T50 Rising Limb Falling Limb Recession Limb Vrecession Vtotal tend • Once an event has be identified on the hydrograph, specific event properties can be analyzed • Event volume, duration, time to peak, etc. can be calculated directly from the observed hydrograph • Trends in event parameters can be explored
  • 45. Peak Event Discharge Station Name Trend Duffins Creek above Pickering East Humber River near Pine Grove East Oakville Creek near Omagh Laurel Creek at Waterloo ↑ Redhill Creek at Hamilton Black Creek near Weston ↑ Etobicoke Creek at Brampton ↑ Etobicoke Creek below QEW ↑ Mimico Creek at Islington ↑ Don River at York Mills ↑ Little Don River at Don Mills ↑ Don River at Todmorden ↑ Rouge River near Markham ↑ Highland Creek near West Hill ↑ Harmony Creek at Oshawa ↑
  • 46. Number of Events per Year Station Name Trend Duffins Creek above Pickering East Humber River near Pine Grove East Oakville Creek near Omagh Laurel Creek at Waterloo Redhill Creek at Hamilton Black Creek near Weston Etobicoke Creek at Brampton ↑ Etobicoke Creek below QEW Mimico Creek at Islington Don River at York Mills ↑ Little Don River at Don Mills ↑ Don River at Todmorden Rouge River near Markham ↑ Highland Creek near West Hill ↑ Harmony Creek at Oshawa ↑
  • 47. Event Volume Station Name Trend Duffins Creek above Pickering East Humber River near Pine Grove East Oakville Creek near Omagh Laurel Creek at Waterloo ↑ Redhill Creek at Hamilton ↑ Black Creek near Weston Etobicoke Creek at Brampton ↑ Etobicoke Creek below QEW ↑ Mimico Creek at Islington ↑ Don River at York Mills ↓ Little Don River at Don Mills ↑ Don River at Todmorden ↑ Rouge River near Markham ↑ Highland Creek near West Hill Harmony Creek at Oshawa
  • 48. Total Event Duration Station Name Trend Duffins Creek above Pickering East Humber River near Pine Grove East Oakville Creek near Omagh ↓ Laurel Creek at Waterloo Redhill Creek at Hamilton Black Creek near Weston ↓ Etobicoke Creek at Brampton ↓ Etobicoke Creek below QEW ↑ Mimico Creek at Islington ↑ Don River at York Mills ↓ Little Don River at Don Mills ↑ Don River at Todmorden ↓ Rouge River near Markham ↑ Highland Creek near West Hill ↓ Harmony Creek at Oshawa ↓
  • 49. Event Quick Flow (Direct Runoff) Volume Station Name Trend Duffins Creek above Pickering East Humber River near Pine Grove East Oakville Creek near Omagh Oakville Creek at Milton ↓ Credit River near Orangeville Black Creek near Weston Etobicoke Creek at Brampton ↑ Etobicoke Creek below QEW ↑ Mimico Creek at Islington ↑ Don River at York Mills Little Don River at Don Mills ↑ Don River at Todmorden Rouge River near Markham ↑ Highland Creek near West Hill ↑ Harmony Creek at Oshawa MK Trend: Increasing
  • 50. Event Interflow Volume Station Name Trend Duffins Creek above Pickering ↑ East Humber River near Pine Grove East Oakville Creek near Omagh Oakville Creek at Milton Credit River near Orangeville Black Creek near Weston ↑ Etobicoke Creek at Brampton Etobicoke Creek below QEW ↑ Mimico Creek at Islington ↑ Don River at York Mills Little Don River at Don Mills ↑ Don River at Todmorden ↑ Rouge River near Markham ↑ Highland Creek near West Hill ↑ Harmony Creek at Oshawa ↑ MK Trend: Increasing
  • 51. Station Name Peak Discharg e Time to Peak Event Duration Total Hydrograp h Duration Event Volume Total Hydrograp h Volume Flashines s Duffins Creek above Pickering East Humber River near Pine Grove East Oakville Creek near Omagh ↓ Oakville Creek at Milton ↑ ↓ ↓ ↓ ↓ ↓ ↑ Credit River near Orangeville ↑ Laurel Creek at Waterloo ↑ ↑ ↑ ↑ ↑ Redhill Creek at Hamilton ↑ Black Creek near Weston ↑ ↓ ↑ Etobicoke Creek at Brampton ↑ ↓ ↓ ↓ ↑ ↑ ↑ Etobicoke Creek below QEW ↑ ↑ ↑ ↑ ↑ ↑ Mimico Creek at Islington ↑ ↑ ↑ ↑ ↑ ↑ Don River at York Mills ↑ ↓ ↓ ↓ ↓ ↑ Little Don River at Don Mills ↑ ↑ ↑ ↑ ↑ ↑ ↑ Don River at Todmorden ↑ ↓ ↓ ↑ ↑ ↑ Rouge River near Markham ↑ ↑ ↑ ↑ ↑ ↑ Highland Creek near West Hill ↑ ↓ ↓ ↓ ↑ ↑ Harmony Creek at Oshawa ↑ ↓ ↓ ↑ Summary (Warm Weather Trends)
  • 52. Mimico Creek at Islington (02HC033) 1970 • Effective Catchment Area - 215 km2 • Urbanized Area - 33.3 km2 (45%) • Total Road Length - 450 km 0 2 4 61 Kilometers Effective Catchment Area Road Network - 1970 Urbanized Area - 1970
  • 53. Mimico Creek at Islington (02HC033) 1978 • Effective Catchment Area - 215 km2 • Urbanized Area - 40.2 km2 (55%) • Total Road Length - 553 km 0 2 4 61 Kilometers Effective Catchment Area Road Network - 1978 Urbanized Area - 1978
  • 54. Mimico Creek at Islington (02HC033) 1995 • Effective Catchment Area - 215 km2 • Urbanized Area – 53.0 km2 (72%) • Total Road Length - 641 km 0 2 4 61 Kilometers Effective Catchment Area Road Network - 1995 Urbanized Area - 1995
  • 55. Mimico Creek at Islington (02HC033) 2005 • Effective Catchment Area - 215 km2 • Urbanized Area - 60.2 km2 (81.5%) • Total Road Length - 683 km 0 2 4 61 Kilometers Road Network - 2005 Effective Catchment Area Urbanized Area - 2005
  • 56. Highland Creek near West Hill (02HC013) 1955 • Effective Catchment Area - 89 km2 • Urbanized Area - 8.9 km2 (10%) • Total Road Length - 248 km 0 1 2 3 40.5 Kilometers Topographic Catchment Boundary Road Network - 1955 Forest Cover - 1955 Urbanized Area - 1955
  • 57. Highland Creek near West Hill (02HC013) 2010 • Effective Catchment Area - 89 km2 • Urbanized Area - 76.5 km2 (86%) • Total Road Length - 876 km 0 1 2 3 40.5 Kilometers Topographic Catchment Boundary Road Network - 2010 Urbanized Area - 2010
  • 58. Change in 1.5 Year Return Discharge 58
  • 59. Change in Bankfull Discharge 59