where the river meets the sea: turbidity maxima in the columbia river estuary matthew espie khalilha...
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![Page 1: Where the River Meets the Sea: Turbidity Maxima in the Columbia River Estuary Matthew Espie Khalilha Haynes](https://reader030.vdocument.in/reader030/viewer/2022032703/56649d0a5503460f949dc506/html5/thumbnails/1.jpg)
Where the River Meets the Sea: Turbidity Maxima in the Columbia River Estuary
Matthew EspieKhalilha Haynes
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Introduction: An Estuary is…
• Partially enclosed, brackish waters• Formed when freshwater bodies meet and mingle with saltwater
from the ocean • Among the most productive environments on earth • An assortment of habitats, in and around the water: salt marshes,
swamps, oyster reefs, mangrove forest, and tidal pools…• Home to thousands of species of mammals, birds, and fish• Coastal regions today are the home for 110 million people and is
expected to increase to 127 million by the year 2010 (http://estuaries.org/)
Washington
Oregon
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Estuarine Turbidity Maxima (ETM)
What Makes an ETM:• ETM are areas of elevated levels of suspended
sediments.• ETM vary in strength and move with the tides.• ETM are thought to be an important factor in the
productivity of estuaries• ETM are the points in the estuary that are most
turbid (opaque)• High biological activity• Provides nutrients for bacteria and smaller animals
at lower trophic levels• Columbia River ETM seems to follow the leading
edge of the salt wedge as it makes its way upstream as the tide is flooding, and then as it retreats during an ebb tide.
(http://depts.washington.edu/cretmweb/CRETM.html)
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Introduction: CMOP
• CMOP’s Vision: To understand and predict the response of coastal margins to human and climate influences
• Focus on the Columbia River and the adjacent Pacific Northwest estuaries
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Objectives
• Find and predict the location of the elusive estuarine turbidity maximum (ETM) for the Columbia River estuary
• Analyze sensor data from the Saturn 01 and 03 systems. Analyze relationships between variables:– Turbidity– Salinity– Chlorophyll– Tide
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Process
Read background information
Explore CMOP database (http://www.stccmop.org/datamart
)
Examine data from multiple stations in the estuary (
http://www.stccmop.org/datamart/station/timeseries
)Import data into Excel
Make plots
Perform correlation analyses
Analyze the different types of tides.
Research ETM.
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Process
Analyze data time series.
Analyze data time series to provide context for previous
research cruises. (http://www.stccmop.org/node/1566
)
Download data from station SATURN01 and graph them in
Excel. Analyze the spikes in turbidity.
Create a diagram of the ETM
Download data from Aug. 2007 cruise where samples were taken
during an ETM.
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Process
Create a program that imports the ETM data into
Matlab.
Import the data into Matlab. Make graphs that show
relationship between turbidity and another variable. Make
graphs of the max turbidity at each station sampled and the corresponding salinity values.
Find peaks in graphs of turbidity, salinity, tides, and change in salinity (include time of
peak).
Find time differences between peaks in each parameter and
peaks in tidal peaks.
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Process
Sort time differences according to tidal type
.
Perform statistical analyses on sets of data.
Redesign sediment distribution maps.
Analyze sediment
distribution trends in regard
to the ETM
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Conclusion and Future Work
• Using the results of the statistical analyses of SATURN01 sensor data, we were able to better predict the timing of the ETM at the sensor location.
• Future statistical analyses should be done over multiple seasons, with a more diverse data and representative data supply, including data from SATURN03.
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THANK YOU!!
We would like to thank our mentors Nirzwan Bandolin, António Baptista, Grant Law, and Karen Wegner and all of our parents for their help and support!...and everyone else at CMOP who also assisted us!
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The Goods: How the ETM works…
http://depts.washington.edu/cretmweb/CRETM.html
At the foot of the salt wedge there is lots of turbulence and mixing of the salt water and the
sediment found on the river bed; the ETM should be close.
Material in the water column is re-suspended and advected
up the salt wedge and dispersed on it’s way to the
ocean.
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August 2007 RV Barnes Research Cruise
Turbidity (NTU) and Salinity (PSU) at Station 22
Turbidity (NTU) and Oxygen (mg/L) at Station 22
Casts Casts
Dep
th (
m)
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August 2007 RV Barnes Research Cruise
Tu
rbid
ity
(NT
U)
Sali
nit
y (P
SU
)
stations
stations
Corresponding Salinity Values
Max Turbidity at each Station
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Time series
0
5
1 0
1 5
2 0
2 5
3 0
1 4 3 8 5 1 2 7 1 6 9 2 1 1 2 5 3 2 9 5 3 3 7 3 7 9 4 2 1 4 6 3 5 0 5 5 4 7 5 8 9 6 3 1 6 7 3 7 1 5 7 5 7 7 9 9 8 4 1 8 8 3 9 2 5 9 6 7 1 0 0 9 1 0 5 1 1 0 9 3 1 1 3 1 1 7 1 2 1 1 2 6 1 3 0 3 1 3 4 1 3 8 1 4 2
-0 .5
0
0 .5
1
1 .5
2
2 .5
3
3 .5
1 9 1 7 2 5 3 3 4 1 4 9 5 7 6 5 7 3 8 1 8 9 9 7 1 0 5 1 1 3 1 2 1 1 2 9 1 3 7 1 4 5 1 5 3 1 6 1 1 6 9 1 7 7 1 8 5 1 9 3 2 0 1 2 0 9 2 1 7 2 2 5 2 3 3 2 4 1 2 4 9 2 5 7 2 6 5 2 7 3 2 8 1
Salinity[psu]
Δ Salinity
Turbidity[NTU]
Tide
Time
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Predicting Turbidity
Type 1 Type 2 Type 3 Type 4
Mean 19.89 16.28 13.27 17.21
Standard Error 1.35 0.97 1.37 1.62
Median 20.69 16.06 13.26 18.11
Standard Deviation 4.06 3.07 3.87 4.85
Range 13.14 9.35 12.87 12.84
Minimum 12.05 12.426 8.17 9.97
Maximum 25.19 21.76 21.04 22.81
Sample Size 9 10 8 9
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Predicting Change in Salinity
Type 1 Type 2 Type 3 Type 4
Mean 5.14 0.86 4.26 0.77
Standard Error 0.11 0.42 0.41 0.09
Median 5.28 0.65 4.17 0.74
Standard Deviation 0.32 1.25 1.1 0.26
Range 0.92 4.53 3.17 0.78
Minimum 4.68 -0.5 3.23 0.3
Maximum 5.6 4.03 6.4 1.08
Sample Size 8 9 7 8
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Predicting Salinity
small large
Mean 0.06 0.07
Standard Error 0.15 0.21
Median 0.23 -0.01
Standard Deviation 0.46 0.67
Range 1.15 2.37
Minimum -0.62 -0.6
Maximum 0.53 1.77
Sample Size 10 10
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What the Numbers Mean…
1 2 3 4
Tide
Time
Heig
ht
(m)
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Sediment Distribution Maps
*
*blue: positively skewed magenta: negatively skewed
South Channel
North Channel
Sedimentary Processes & Environments in the Columbia River Estuary
C. Sherwood J. Creager E. Roy G. Gelfenbaum T. Dempsey
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Sediment Distribution Maps
Sedimentary Processes & Environments in the Columbia River Estuary
C. Sherwood J. Creager E. Roy G. Gelfenbaum T. Dempsey
*blue: positively skewed magenta: negatively skewed
*
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Time series
Time
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Tides
Time
Slack tide Ebb tideFlood tide
Heig
ht
(m)
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24Graphs and Analyses
TIME
TIME
Salinity is high when tubidity is low.
Turbidity has a pattern: low spike, high spike… high spike, low spike,… etc
Turbidity pattern coincides with flood and ebb tides.
June 1-11, 2008
June 1
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The Estuary