HomeMy WebLinkAboutExh.25_CMZ_Risk_Assessment750 Sixth Street South | Kirkland, WA 98033 | P 425.822.5242 | f 425.827.8136 | watershedco.com
TECHNICAL REPORT
Date: April 8, 2020
To: Matt Herrera
From: Alan Wald, LHg
Project Name: Cedar River Apartments
Project Number: 170314
Subject: C hannel Migration Risk Assessment Memo
The following report includes review of hydrologic indicators, geomorphic indicators, and
historical records relevant to potential CMZ hazards on a lower Cedar River reach from River
Mile (RM) 1.75 to 2.5.
L ocation
The location of the proposed Cedar River Apartments (Project Site, parcel #1723059026), is
located on the right bank upstream of I-405, as shown in Figure 1 (King County iMap, 2020a).
Figure 1. Project site on the Cedar River near Renton, WA
EXHIBIT 25
RECEIVED
08/13/2020 MHerrera
PLANNING DIVISION
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The Watershed Company
Channel Migration Risk Assessment
April 8, 2020
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H ydrologic Indicators
The Cedar River drains an area of 184 square miles from the foothills of the Cascade Mountains
to Lake Washington and Puget Sound. River discharge (flow) is regulated by Seattle City Light
Masonry Dam built in 1914 for hydropower, water supply, and flood control. Frequency
analysis of peak flow on the Cedar River near Renton (NHC, 2018b) is reported to be:
• 2-year flow of 3000 cubic feet per second (cfs),
• 5-year flow of 4600 cfs
• 10-year flow of 5940 cfs,
• 50-year flow of 9860 cfs
• 100-year flow of 12,000 cfs
Annual peak flow of record varies from less than 2,000 cfs to 10,600 cfs, as shown in Table 1 and
Figure 2. (USGS, 2020).
Period
Peak Flow
Rate (cfs)
Return Period
(years)
1985 - 1991 10,600 50 – 100
1991 - 1997 7,650 10 – 50
1997 - 1998 1,920 <2
1998 - 1999 2,840 <2
1999 - 2000 2,890 <2
2000 - 2001 1,100 <2
2001 - 2002 2,620 <2
2002 - 2003 2,060 <2
2003 - 2004 2,510 <2
2004 - 2005 2,410 <2
2005 - 2006 4,380 2 – 10
2006 - 2007 6,090 10 – 50
2007 - 2008 2,980 <2
2008 - 2009 9,470 10 – 50
2009 - 2010 2,120 <2
2010 - 2011 5,870 2 – 10
2011 - 2012 2,790 <2
2012 - 2013 3,860 2 – 10
2013 - 2014 2,800 <2
2014 - 2015 5,500 2 – 10
2015 - 2016 2,500 <2
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The Watershed Company
Channel Migration Risk Assessment
April 8, 2020
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2017 - 2018 2,330 <2
2018 - 2019 2,370 <2
2019 - 2020 9,620 10 – 50
Table 1. Annual peak flow. Cedar River at Renton, WA
Figure 2. Graph of annual peak streamflow. Cedar River at Renton WA.
Peak flows in excess of 6,000 cfs (10-year return interval flow) at this site are considered channel
forming flow of sufficient depth, velocity, and stream power to initiate channel migration by
rapid meandering and channel avulsion (WDFW, 2009). There have been seven of these channel
forming flows on the lower Cedar River since Water Year (WY) 1940, not including a major dam
break flood in 1911, as follows:
WY1966 7,650 cfs
WY1972 6,201 cfs
WY1976 8,800 cfs
WY1991 10,600 cfs
WY2007 6,090 cfs
WY2009 9,390 cfs
WY2020 9,620 cfs
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The Watershed Company
Channel Migration Risk Assessment
April 8, 2020
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G eomorphic Indicators
The Cedar River downstream of I-405 is a constructed, reinforced channel with no meanders.
Aggradation of bed sediments is controlled by regular dredging and the channel is fixed in
place by the I-405 abutments and bank revetments (NHC, 2019). Effects of channel constriction
by the I-405 abutments extends upstream and potential channel meanders are constrained by
outlet control through the bridge.
The Cedar River upstream of I-405, for about 2 miles to Maplewood Subdivision and Soos
Creek Park, is an incised reach with narrow, irregular meanders, hardened banks, and several
industrial developments on the shoreline. Almost every outside bend is armored by levees and
revetments or bounded by an erosion-resistant feature (KC, 2015). Erosion control projects for
the Milwaukee Railroad mainline (now Cedar River Trail), SR169 (Maple Valley Highway), and
King County levees and revetments at Riverview Park limit the width of the channel and
disconnect the river from its floodplain. Woody debris loading is very low and sediment
transport exceeds sediment supply in the reach (NHC, 2018; KC, 2015). Average meander width
is about half the unconstrained (historical) meander width and average channel bed elevation
varied by less than 1.0 ft from 1985 to 2020 (NHC, 2019).
The riverbank at the project site is protected from erosion by a massive concrete revetment built
sometime around 1961, as shown in Figure 3. The revetment was not affected by six floods,
ranging from 6,090 cfs to 10,600 cfs, from WY1996 to WY2009.
Figure 3. Concrete revetment at the project site
RM 1.75 - 2.5 upstream of I-405
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The Watershed Company
Channel Migration Risk Assessment
April 8, 2020
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H istorical Record
Aerial photographs show no side channel development, channel avulsion, or significant bank
erosion on the project site for 82 years (since 1938). LiDAR imagery (KC, 2020) show no side
channels or meander scars on the project site, including after the WY1991 flood of 10,600 cfs, as
shown in Figure 4 (KC, 2020b).
Figure 4. LiDAR image of project site on right bank of Cedar River upstream of I-405
S ummary
Department of Ecology guidelines for delineation of channel migration zones (WDOE, 2003)
include assessment of the Historical Migration Area (HMA), Avulsion Hazard Area (AHA),
Erosion Hazard Area (EHA), and Disconnected Migration Areas (DMA). There are no
geomorphic or photogrammatic indicators of an HMA on the project site for more than 100
years since the dam was built. There is no AHA or EHA mapped on the Cedar River
downstream of RM 5.0 (KC, 2015. Table 6 and Map 5), as shown in Figure 5.
DocuSign Envelope ID: 99BA427F-FE67-49CC-B142-9BE0760232C1
The Watershed Company
Channel Migration Risk Assessment
April 8, 2020
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Figure 5. Map of potential CMZ features on the lower Cedar River
Published estimates of channel widening by bank erosion (KC, 2015, Appendix B) are for
unarmored areas and would not apply to the project site. There is no evidence of a DMA on the
project site. Although the project site is mapped as a severe hazard area (KC, 2015. Map7),
shown in Figure 6 below, the delineation appears to be a projection of a mapping algorithm
unverified by the necessary field investigation and site surveys.
DocuSign Envelope ID: 99BA427F-FE67-49CC-B142-9BE0760232C1
The Watershed Company
Channel Migration Risk Assessment
April 8, 2020
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Figure 6. Map of potential CMZ classifications on the lower Cedar River
Based on hydrologic, geomorphic, and photogrammatic information contained in this report,
there is no quantitative information to suggest there is a channel migration hazard on the
project site today.
Sincerely,
Alan R. Wald, LHg
DocuSign Envelope ID: 99BA427F-FE67-49CC-B142-9BE0760232C1
DocuSign Envelope ID: 99BA427F-FE67-49CC-B142-9BE0760232C1
750 Sixth Street South | Kirkland, WA 98033 | P 425.822.5242 | f 425.827.8136 | watershedco.com
R eferences
(KC, 2020a). King County. King County Parcel Viewer.
https://kingcounty.gov/services/gis/Maps/parcel-viewer.aspx
(KC 2020b). King County. LiDAR Swipe. https://www5.kingcounty.gov/lidar/
(KC, 2015). King County. Cedar River Channel Migration Study. Prepared by Terry Butler and
Fred Lott. King County Department of Natural Resources and Parks, Water and Land Resources
Division. Seattle, Washington. 2015
(NHC, 2018a). Northwest Hydraulic Consultants, Inc. Cedar River 2018 Annual Sediment
Report. Final Report. Prepared for City of Renton, WA. Seattle, WA. December, 2018
(NHC, 2018b). Northwest Hydraulic Consultants, Inc. Cedar River 2017 Annual Sediment
Report. Final Report. Prepared for City of Renton, WA. Seattle, WA. January, 2018
(NHC, 2019). Northwest Hydraulic Consultants, Inc. Post-Dredge Cedar River Scour
Monitoring Report. Memo Report. Prepared for City of Renton, WA. Surface Water Utility.
Seattle, WA. March, 2019
(USGS,2020). US Geological Survey. Surface Water Data for Washington State. Station
#12119000 https://waterdata.usgs.gov/wa/nwis/rt
(WDOE, 2003). Washington Department of Ecology. A Framework for Delineating Channel
Migration Zones. Prepared by Cygnia Rapp and Timothy Abbe. In cooperation with
Washington Department of Transportation. Ecology Publication #03-06-027. Olympia, WA.
November, 2003.
(WDFW, 2009). Washington Department of Fish and Wildlife. High Flows for Fish and Wildlife
in Washington. Report of Investigations in Instream Flows. Prepared by Alan Wald, Habitat
Program. Olympia, WA. 2009
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