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Effective Discharge Nooksack Watershed
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Leif Embertson
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Effective Discharge Nooksack Watershed
1.
Recent trends in
effective discharge in Northwest Washington R. Leif Embertson, MS, PE River Restoration Northwest Conference February 1st , 2011
2.
3.
4.
5.
6.
7.
8.
9.
NOOKSACK RIVER AT
FERNDALE (LOWER WATERSHED)Objective Definition Study Area Methods Results Next Steps Discussion
10.
11.
12.
Bin Size and
Type
13.
Arithmetic vs log
14.
Sediment Transport (Observed
or Equations)
15.
If equations, Hydraulics
R=aQb
16.
Sensitivity analysisObjective Definition
Study Area Methods Results Next Steps Discussion
17.
RESULTS Objective Definition
Study Area Methods Results Next Steps Discussion UPPER WATERSHED
18.
RESULTS Objective Definition
Study Area Methods Results Next Steps Discussion LOWER WATERSHED
19.
20.
Changes in upper
watershed are more significant than in lower watershed
21.
Effective discharge (Qeff)
22.
Annual sediment loadObjective
Definition Study Area Methods Results Next Steps Discussion
23.
24.
Recent hydrologic patterns
will/are causing a channel response
25.
Upper watershed(s) are
likely to be directly affected and changes more significant (increase in width/depth)
26.
Prepare for a
excess sediment to be delivered to lowland areasObjective Definition Study Area Methods Results Next Steps Discussion
27.
28.
a long term
trend?
29.
a cyclic pattern
within geologic record?
30.
statistical noise?Objective Definition
Study Area Methods Results Next Steps Discussion
31.
32.
Couple with habitat
flow parametersObjective Definition Study Area Methods Results Next Steps Discussion
33.
THANK YOU [INSERT
PHOTO HERE] Objective Definition Study Area Methods Results Next Steps Discussion
Notes de l'éditeur
Geomorphic paradigm; which events do the most work in shaping a channel and floodplain. Large infrequent events or smaller more frequent events