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Relation of Physical Measures of Streamflow Conditions to Ecological Effects of Urbanization in Streams USGS Jeffrey Steuer; Middleton, WI Krista Stensvold; Middleton, WI Elise Giddings; Raleigh, NC Jerad Bales; Raleigh, NC

USGS Jeffrey Steuer; Middleton, WI Krista Stensvold; Middleton, WI Elise Giddings; Raleigh, NC

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Relation of Physical Measures of Streamflow Conditions to Ecological Effects of Urbanization in Streams. USGS Jeffrey Steuer; Middleton, WI Krista Stensvold; Middleton, WI Elise Giddings; Raleigh, NC Jerad Bales; Raleigh, NC. Explanaton. WMIC EUSE Study Area. WMIC Study Unit. Water. - PowerPoint PPT Presentation

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Page 1: USGS Jeffrey Steuer; Middleton, WI Krista Stensvold; Middleton, WI Elise Giddings; Raleigh, NC

Relation of Physical Measures of Streamflow Conditions to Ecological Effects of Urbanization in Streams

USGSJeffrey Steuer; Middleton, WI

Krista Stensvold; Middleton, WI

Elise Giddings; Raleigh, NC

Jerad Bales; Raleigh, NC

Page 2: USGS Jeffrey Steuer; Middleton, WI Krista Stensvold; Middleton, WI Elise Giddings; Raleigh, NC

National Water-Quality Assessment (NAWQA)

Program Effects of urbanization on

stream ecology

Explanaton

WMIC EUSE Study Area

WMIC Study Unit

Water

Streams

Final watersheds

Urban Index I

80-100

60-80

40-60

20-40

0-20

Milwaukee-Green Bay 30 Watersheds

Page 3: USGS Jeffrey Steuer; Middleton, WI Krista Stensvold; Middleton, WI Elise Giddings; Raleigh, NC

Milwaukee-Green Bay – range of urbanization30 Watersheds

Watershed Size Range = 5 – 39 mi2

Urban land cover Range = 3- 99 percent

Proportion population change 1990 – 2000 Range = -0.16 – 1.38

Page 4: USGS Jeffrey Steuer; Middleton, WI Krista Stensvold; Middleton, WI Elise Giddings; Raleigh, NC

Problem review

• Compare two time series data foundations for response to urbanization and association to stream biology.

1. Hydraulic variables (HEC); simulated hydraulic variables estimate direct stream conditions such as velocity, depth, shear stress, turbulence, bed exposure.

2. Hydrologic condition metrics (HCM); measures patterns of flow conditions during different time periods (magnitude, duration and freq of high, low flow and flow change).

Page 5: USGS Jeffrey Steuer; Middleton, WI Krista Stensvold; Middleton, WI Elise Giddings; Raleigh, NC

Eleven transects per ~150 m reach…..

15m

Rio (UII=10)Mapped imp = 1%

Hoods (UII=31)Mapped imp = 6%

Jambo (UII = 0)Mapped imp = 1%

Lincoln (UII=100)Mapped imp = 45%

Garners (UII=60)Mapped imp = 26%

Fox (UII=40)Mapped imp = 6%

Page 6: USGS Jeffrey Steuer; Middleton, WI Krista Stensvold; Middleton, WI Elise Giddings; Raleigh, NC

Transect measurements of instream and channel

conditions……

1.Bankfull width

2.Wetted channel width

3.Depth & velocity 1

2

3ThalwegFitzpatrick; modified

Page 7: USGS Jeffrey Steuer; Middleton, WI Krista Stensvold; Middleton, WI Elise Giddings; Raleigh, NC

Transect measurements of streambank characteristics…..

4.Bank angle

5.Bank height

(bankfull

depth)

4

5

Page 8: USGS Jeffrey Steuer; Middleton, WI Krista Stensvold; Middleton, WI Elise Giddings; Raleigh, NC

First data foundation – Hydraulic (HEC) variable

time series….

• Build upon habitat geometry, reach map, photographs, reach gradient (water surface slope at low Q)

• Hydrograph (daily and hourly)

Page 9: USGS Jeffrey Steuer; Middleton, WI Krista Stensvold; Middleton, WI Elise Giddings; Raleigh, NC

Energy balance – transect to transect

Unsteady –storage, mass balance

Page 10: USGS Jeffrey Steuer; Middleton, WI Krista Stensvold; Middleton, WI Elise Giddings; Raleigh, NC

Hydraulic model (Hec-Rasv3.1.2)

• Limitations/assumptions:– Crude cross section data, estimated overbank slope– Rough elevation data– One dimensional (no lateral velocity gradient)

• HEC model output - hydraulic variable time series for 11 transects – annual period of record (POR) and three seasons.– Flow– Wetted perimeter– Depth– Velocity– Stream power– Froude number– Water column Reynolds number– Bottom shear stress

~ 10,000 time series (30 sites, 8 variables, 11 transects, 4 POR)

Page 11: USGS Jeffrey Steuer; Middleton, WI Krista Stensvold; Middleton, WI Elise Giddings; Raleigh, NC

Bottom shear stress for 11 transects at OAK Creek Each reach aggregated into a max, min, average value

Summer POR

Page 12: USGS Jeffrey Steuer; Middleton, WI Krista Stensvold; Middleton, WI Elise Giddings; Raleigh, NC

Maximum shear stress at 11 Oak Creek transects; two adjacent transects with lowest peak shear - variable “refug.2”

Page 13: USGS Jeffrey Steuer; Middleton, WI Krista Stensvold; Middleton, WI Elise Giddings; Raleigh, NC

Maximum shear stress at transects for 25 streams two transect refuge denoted in red

Summer POR

Transects

Page 14: USGS Jeffrey Steuer; Middleton, WI Krista Stensvold; Middleton, WI Elise Giddings; Raleigh, NC

Hydraulic model time series variables (continued…)

1. Refuge concept (shear) – Minimum shear stress in a “refuge” (2,3,4,5,6 adjacent transects) for a range of sizes

2. Exceed a threshold (shear)- Duration and integration of shear stress above a threshold (1, 2, 5, 20, 100 dyne/cm2)

3. Fraction exposed bed – estimated from wetted perimeter time series and fixed bed width (photos/survey)

Additional variables derived from the HEC generated time series

Page 15: USGS Jeffrey Steuer; Middleton, WI Krista Stensvold; Middleton, WI Elise Giddings; Raleigh, NC

Example hydraulic (HEC) variable relations

Invertebrate - Filter collector richness increased with minimum shear stress

March 2004

8

10

12

14

16

18

20

0 10 20 30 40 50

Minimum shear stress; reach averaged (min.tau; dyn/cm2)

Filt

er C

olle

ctor

Ric

hnes

s (Q

_FC

) .

R2 = 0.58

fall (hourly)

R2 = 0.35

0

0.05

0.1

0.15

0.2

0.25

0.3

0.35

0.4

0.45

0.5

0.00 0.05 0.10 0.15 0.20Fraction of exposed bed

R_

Gu

ild 8

_rA

.

R_Guild 8

Log.(R_Guild 8)

Decreased motile algae with increase amount of exposed bed

Biological metrics we’ve selected - Not assemblages in a multivariate fashion but do represent measures of communities which are meaningful (metrics that could be measured in a biomonitoring program).

Page 16: USGS Jeffrey Steuer; Middleton, WI Krista Stensvold; Middleton, WI Elise Giddings; Raleigh, NC

Example hydraulic (HEC) variable relations continued..

Fall (hourrly)

0

10

20

30

40

50

60

0 20 40 60 80 100 120 140 160 180 Two transect refuge (refuge.2; dyne/cm2)

Fis

h IB

I

Fish IBI

Log. (FishIBI)

R2 = 0.46

Fish IBI had negative association with increased shear stress in the two transect refuge

Refuge.2 bottom shear stress increased with urban intensity index

Fall (hourly)

Fish IBI – Lyons et al., 1992

Page 17: USGS Jeffrey Steuer; Middleton, WI Krista Stensvold; Middleton, WI Elise Giddings; Raleigh, NC

Second data foundation…..

Hydrologic Condition Metrics (HCM)- measure patterns of flow conditions during different time periods (magnitude, duration and freq of high, low flow and flow change).

[modified from Nature Conservancy indicators of hydrologic alteration (IHA)]

Page 18: USGS Jeffrey Steuer; Middleton, WI Krista Stensvold; Middleton, WI Elise Giddings; Raleigh, NC

Examples of hydrologic condition metrics (HCMs).

Area normalized hydrographs for a low and high UII site. Arrows indicate rises that area (flow) was seven times the median rise (PERIODR7). Pigeon had seven rises; Pokeberry had three rises.

Fm Giddings; in review

Page 19: USGS Jeffrey Steuer; Middleton, WI Krista Stensvold; Middleton, WI Elise Giddings; Raleigh, NC

Hydrologic condition metrics (HCMs) continued...Example of duration metric

Storm hydrograph for a low and high UII site. Shaded area is portion of hydrograph above the 90 percent flow value (MDH90). Pigeon was 11 hrs;

Pokeberry was 43 hrs.

Fm Giddings; in review

Page 20: USGS Jeffrey Steuer; Middleton, WI Krista Stensvold; Middleton, WI Elise Giddings; Raleigh, NC

Hydrologic condition metric (HCM) – biologic relations

Invertebrate - EPT abundance had negative correlation with flow variation

Diatom richness decreased with the duration of low flow during fall POR

Fall (hourly)

R2 = 0.46

30

35

40

45

50

55

60

65

70

75

80

0 5 10 15 20 25 30Median duration of low flow (hrs; MDL_5)

D.d

tm.R

ich

.

D.dtm.Rich

Log.(D.dtm.Rich)

Page 21: USGS Jeffrey Steuer; Middleton, WI Krista Stensvold; Middleton, WI Elise Giddings; Raleigh, NC

Hydrologic condition metric (HCM) relations continued..

Fish IBI decreased with stream flashiness in the fall POR.

Fall (hourly)

R2 = 0.63

0

10

20

30

40

50

60

0 0.2 0.4 0.6 0.8 1 1.2 1.4

Richard_Baker flashiness index (rb_flash)

Fis

h IB

I .

Fish IBI

Linear(FishIBI)

With increased urbanization the duration of high flow (exceeded 10% of the time) was shorter.

Page 22: USGS Jeffrey Steuer; Middleton, WI Krista Stensvold; Middleton, WI Elise Giddings; Raleigh, NC

Hourly based metrics (HCM and HEC) computed over 3 intervals (hourly data) and annual POR (daily data)

Low UII

0

100

200

300

400

500

600

700

800

900

1,000

10/01/03 12/01/03 01/31/04 04/01/04 06/01/04 08/01/04 10/01/04

Black Creek (hr)

Black (daily)

Hourly data- missing

0

200

400

600

800

1,000

1,200

1,400

1,600

1,800

2,000

10/1/03 12/1/03 1/31/04 4/1/04 6/1/04 8/1/04 10/1/04

Lincoln Creek (hr)

Lincoln (daily)

High UII

Spring 2004

summer 2004fall 2003

Flo

w/a

rea

Flo

w/a

rea

Page 23: USGS Jeffrey Steuer; Middleton, WI Krista Stensvold; Middleton, WI Elise Giddings; Raleigh, NC

Mean spearman correlation coefficients (absolute value) for 37 biologic endpoints

[Hydrologic condition metric (HCM); Hydraulic model variable (HEC)]

Overall… HCM relations ~15% stronger than HEC

Blue value is maximum correlation within a group

CHANGE HYD to HEC…

Page 24: USGS Jeffrey Steuer; Middleton, WI Krista Stensvold; Middleton, WI Elise Giddings; Raleigh, NC

Fish IBI regression tree model build on hydraulic variable data foundation (daily data, annual POR)

Page 25: USGS Jeffrey Steuer; Middleton, WI Krista Stensvold; Middleton, WI Elise Giddings; Raleigh, NC

Fish IBI regression tree model build on hydrologic condition metric foundation (daily data, annual POR)

Page 26: USGS Jeffrey Steuer; Middleton, WI Krista Stensvold; Middleton, WI Elise Giddings; Raleigh, NC

Hydrologic condition metric (HCM) tree regression models ~ 8% stronger (lower deviation) than hydraulic (HEC) variable models….. consistent with correlation results.

• However hydraulic variables offer potential link between reach scale change and biologic endpoint….

BLOT

Page 27: USGS Jeffrey Steuer; Middleton, WI Krista Stensvold; Middleton, WI Elise Giddings; Raleigh, NC

And a possible understanding to biologic mechanism…..

Field experiment in 27 patches in 150 m reach – northeastern Spain. Examined invertebrate loss from bed with shear stress. Gibbins et al.; 2007.

Page 28: USGS Jeffrey Steuer; Middleton, WI Krista Stensvold; Middleton, WI Elise Giddings; Raleigh, NC

Invertebrate drift became exponential at shear stress of 9 dyne/cm2 …..

Gibbins et al.; 2007

Page 29: USGS Jeffrey Steuer; Middleton, WI Krista Stensvold; Middleton, WI Elise Giddings; Raleigh, NC

Our hydraulic modeling of refuge bottom shear stress at 25 sites is consistent with that finding…..

Scraper abundance decreased with increasing shear stress in refug.2

0

5

10

15

20

25

30

35

40

45

100 600

R_S

C

Summer; maximum shear in refug.2

0

5

10

15

20

25

30

35

40

45

0 10 20 30 40 50 60 70 80 90 100Shear stress (dyn/cm2)

R_S

C_

pa .

refuge (2)

9 dyn/cm2

Page 30: USGS Jeffrey Steuer; Middleton, WI Krista Stensvold; Middleton, WI Elise Giddings; Raleigh, NC

findings to date

• A 1- dimensional hydraulic model, based on the NAWQA habitat data and flow record, allowed us to examine hydraulic and habitat conditions throughout the water year.

• Time series based hydrologic condition metrics (HCM) and hydraulic variables (HEC) had numerous significant biologic relations (algae, invertebrates, fish) across all POR.

• HCM data foundation had stronger association with biology than the hydraulic data foundation. – Both foundations may provide link between watershed

scale change and stream biology.

• Hydraulic variables may provide mechanistic insight and provide a link between reach scale change (restoration) and biology.

Page 31: USGS Jeffrey Steuer; Middleton, WI Krista Stensvold; Middleton, WI Elise Giddings; Raleigh, NC

Acknowledgements…..many, many people

• Study design and management– Cathy Tate, Jerry McMahon, Tom Cuffney

• Site installations and hydrology data collectors• Habitat and biology data collectors• Data processing – biology, hydrology, habitat• Hec-Ras model (30) construction and output

processing

Many skill sets/backgrounds required…..

USGS/NAWQA able to provide framework