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Kieser & Associates, LLC 536 E. Michigan Ave. , Suit e 300, Kalamazoo, MI 49007
page 1
To: Cedar Lake Improvement Lake Board Date: May 22, 2017
From: Brian Boyer, K&A
Mark Kieser, K&A cc: Doug Pullman, Aquest
RE: Findings for 2016 Cedar Lake Groundwater/Surface Water Level Monitoring
This memorandum presents 2016 results compiled by Kieser & Associates, LLC (K&A)
related to the ongoing water level monitoring program at Cedar Lake, Alcona and Iosco
Counties, Michigan. K&A staff were authorized to continue management and oversight
of ongoing data collection efforts in 2016 on behalf of the Lake Board. The purpose of
the long-term monitoring program is to best understand critical needs and relevant
influences on water levels in Cedar Lake.
Desirable summer month water levels in Cedar Lake are a function of both rainfall and
other management strategies that will support water level maintenance in dry summer
months. The latter efforts, as defined in the approved Cedar Lake Watershed
Management Plan (WMP) relate to bolstering water retention in the northwest cedar
swamp from winter and spring months extending into summer months. This will be
accomplished by improving water controls at the King’s Corner Culvert to reduce out-of-
watershed losses, improving Sherman and Jones Creek water retention using instream
grade structure controls, and utilizing deep groundwater withdrawal augmentation wells
as per the WMP. Water level data being collected for Cedar Lake are vital to assessing,
understanding and cost-effectively pursuing these water level control options in a phased
manner.
Program Background
A volunteer water level monitoring program was initially developed at select
groundwater and surface water monitoring sites around Cedar Lake in 2004. Since then,
these water level monitoring efforts have expanded to include additional critical areas
using automated water level logger equipment in lieu of intermittent volunteer
measurements. The 2016 water level monitoring program included 23 level loggers
located around the lake (Figure 1). Consistent with previous years, a combination of
surface water stations along with shallow and deep groundwater stations were monitored
to document surface/groundwater interactions and their influence on Cedar Lake water
levels. Sherman Creek, Jones Creek and the King’s Corner road culvert were likewise
included in the 2016 monitoring program to assist with calculating estimates of creek
flows in and out of Cedar Lake, as well as culvert flows out of the northwest cedar
TECHNICAL
MEMORANDUM
ENVIRONMENTAL SCIENCE & ENGINEERINGKIESER ASSOCIATES
Kieser & Associates, LLC 536 E. Michigan Ave. , Suit e 300, Kalamazoo, MI 49007
page 2
swamp away from the lake. Rain gage data collected and submitted by Rex Vaughn were
evaluated and used to assess rainfall for 2016 and compared with past rainfall records.
During a period of gage malfunction in June and July, other nearby precipitation data
were gathered from the Harrisville, MI CO-OP Station (#203628) in Alcona County.
2016 Precipitation and Water Level Data
The 2016 water level data from the nearshore groundwater monitoring sites 1-7, along
with Cedar Lake water levels, are graphically illustrated in Figures 2-8. Sites 1, 3, 4, 5
and 6 (Figures 2, 4, 5, 6 and 7, respectively) are in areas where groundwater is moving
away from the lake, as reflected in the 2016 piezometer water levels that were below the
lake water level. Sites 2 and 7 (Figures 3 and 8, respectively) are located in areas where
groundwater is entering the lake, with piezometer groundwater levels near or above those
measured in the lake. Site 2, located nearest the wetland complex northwest of the lake,
signifies why this area is an important groundwater source to the lake and further
emphasizes the importance of wetland protection in this critical area. (Note: during the
2016 monitoring season, the level logger equipped within PZ-2d ceased to operate
correctly. Fortunately, the manufacturer was able to extract the data, however, this 7-year
old level logger will be replaced in 2017). Sites 8-11 (Figures 9-12, respectively)
document conditions beyond the lake toward the southeast within an area of Lakewood
Shores that is well-drained. Water level data for these four sites continue to confirm
shallow groundwater loss to Lake Huron with increasing distance from the Lake.
Historic summer precipitation totals for the Cedar Lake area are presented in Figure 13.
These data represent precipitation information available from the Harrisville, MI CO-OP
Station (#203628), the Oscoda, MI Wurtsmith Airport Station (#14808), and a rain gauge
installed at Cedar Lake and monitored by volunteers. Available rainfall data from 1998-
2016 (minus 2006 when there were no local functioning rain gauges) reflect an 18-year
summer average (June-September) of 12.14 inches of rainfall. The observed 2016 data
are average for rainfall, measuring 12.18 inches during these summer months. The
previous 2015 summer exhibited just below-average summer precipitation amounting to
10.94 inches. Rainfall in 2014 was above average, while 2012 and 2013 were below-
average. The years 2008-2011 each had summer precipitation recorded above-average.
More importantly, with respect to rainfall, the Cedar Lake Augmentation Feasibility
Study completed by K&A in 2011 revealed that in order to avoid water level decreases
greater than 3-inches/month during the critical summer months (June-September), an
average summer month rainfall of 2.75 inches would be necessary. In other words, if
natural rainfall patterns result in less than 2.75 inches in a given summer month, a lake
level drop of approximately 3 inches or more can be expected. Likewise, a June-
September average of 11 inches of rainfall (i.e., 2.75 inches multiplied by 4 months) can
Kieser & Associates, LLC 536 E. Michigan Ave. , Suit e 300, Kalamazoo, MI 49007
page 3
be used to assess each summer season as a whole with regards to desired lake level
conditions. This target threshold is plotted on Figure 13 for sake of comparison.
The 2016 level logger data near the Cedar Lake outflow structures demonstrate that the
lake had water levels greater than the established legal lake level of 608.64 feet for most
of the year (representing lake outflow conditions). The most notable drops below the
legal lake level occurred in August and October. The 2016 Cedar Lake water levels were
plotted with April-November recorded rainfall (Figure 14) to observe lake level response
to local precipitation. As previously noted, and illustrated in Figure 14, the local
precipitation has a direct impact on Cedar Lake water levels with observed responses
corresponding to local rain events. Consistent with the target rainfall threshold data
plotted on Figure 13 (i.e., 11 inches per summer season), Figure 14 shows that early
season to mid-summer 2016 Cedar Lake water levels remained above the legal lake level,
though steadily declining from March to August, then remaining relatively steady
through November. Lake levels remained within a few inches of the northern lake
outflow structures throughout the later portion of the monitoring period. Due to the
relatively small size of the Cedar Lake watershed contributing area, summer rainfall is an
important factor in maintaining Cedar Lake levels. Those years with below-average
rainfall result in significant drops in Cedar Lake water levels as water losses exceed water
gains to the lake.
2016 Estimated Surface Flows
Water level loggers located at the lake outflow area (north end), Sherman Creek, Jones
Creek and King’s Corner culverts (west side of the lake) were used to monitor incoming
and outgoing surface flows of the lake. Both Jones Creek and Sherman Creek are
significant sources of incoming surface water flows to the lake from the wetland complex
northwest of Cedar Lake. On the other hand, the King’s Corner road culvert diverts water
from the immediate watershed to the south, toward Phelan Creek and Van Etten Lake,
resulting in water loss from the Cedar Lake watershed that would otherwise help support
desired Cedar Lake water levels.
The two Cedar Lake outflow structures at the north end of the lake discharge to Lake
Huron once water levels exceed the legal lake level. Figures 15-18 illustrate estimated
surface inflows and outflows associated with Cedar Lake for spring and summer 2016 at
these four monitoring locations. All flow monitoring data are derived from long-term
water level stage-discharge relationships specific to each location. Flow data from all
four of these critical locations were combined and plotted together as illustrated on
Figure 19.
The Jones Creek and Sherman Creek monitoring data reveal inflows of 648 and 922
million gallons (Mgal), respectively, into Cedar Lake from March 21 to July 22, 2016
(refer to Figure 19). These flows are significantly greater than flows in 2015 during a
Kieser & Associates, LLC 536 E. Michigan Ave. , Suit e 300, Kalamazoo, MI 49007
page 4
similar time period. Measured outflow volume leaving Cedar Lake also exceeded 2015
outflows, totaling 2,621 Mgal during this time period, with discernible lake outflows
continuing through the monitoring season. During the same time period, March to July,
185 Mgal flowed out of the Cedar Lake watershed via the King’s Corner road culvert.
Figure 20 summarizes observed flows associated with the Kings Corner culvert location.
The total plotted flows from March 21 to November 18, 2016 reflect a total volume of
216 Mgal over 243 days. This outflow is significantly more than the data observed in
2015 (46.3 Mgal) during a similar period. It is important to keep in mind that these flows
reflect "lost inflow" volume to Cedar Lake. For this reason, we continue to recommend
moving forward with planned property improvements on the newly acquired Lake Board
property to further mitigate losses. The maximum observed high water elevation at the
Kings Corner culvert in 2016 was 610.3. The proposed berm project spillway is set to
overflow at elevation 611.0 feet.
Of important note to surface water inflows to the lake, a total of six railroad culverts
passing beneath the Lake State Railway within the northwest wetland complex area were
given specific maintenance attention by railroad representatives in August/September of
2014. These efforts have since restored wetland surface water flow from the west to the
east beneath the railroad tracks at six culvert locations. The 2016 data confirm our
expectation that these actions have allowed more surface water to consequently pass to
the lake via Sherman and Jones Creeks. Surface water will continue to be lost, however,
through the King’s Corner culvert until a water level control berm can be implemented on
the Lake Board parcel.
Conclusions and Recommendations
Data from 2016 lake level monitoring continue to demonstrate how Cedar Lake first and
foremost responds quite directly to prevailing summer month rainfall amounts. Lake
levels for 2016 appear to have been within the WMP desired levels; this largely being a
function of rainfall similar to the observed historic average for June through September.
Lake outflow data and lake levels still suggest that 2016 lake levels were adequate for
targeted summer conditions, especially considering a partial removal of a beaver dam at
the lake outflow location. The 2014 railroad culvert cleanouts appear to have provided
additional surface flows, as well as late season groundwater recharge benefits into the
northwest cedar swamp. These surface flows may be indicative of the improved surface
connections with the cedar swamp located on the west side of the railroad tracks. The
2016 data also demonstrate a significant increase in the volume of water lost through the
King’s Corner culvert. As a result, lost outflow at Kings Corner could be even further
reduced with a water control berm.
Based on 2016 observations and the noted importance of scientifically valid water level
data for making informed watershed (water level) management decisions, we recommend
Kieser & Associates, LLC 536 E. Michigan Ave. , Suit e 300, Kalamazoo, MI 49007
page 5
the Cedar Lake monitoring program be continued during the 2017 calendar year. Such
data will be vital to maintaining a comprehensive and unbroken historic water level
record. These data will be used to further evaluate: 1) Sherman Creek instream grade
control structure needs within the recently Lake Board-acquired properties surrounding
this creek, 2) King’s Corner impacts and potential water level control berm design and
maintenance needs, 3) potential future benefits with grade control structures in Jones
Creek, and 4) the future need for installing an augmentation well. These latter two items
will only become relevant after the first two items are implemented.
Lastly, we recommend that the Jones Creek monitoring station be removed temporarily
during an upcoming Alcona County Road Commission project along West Cedar Lake
Road. Once the road work is complete, this monitoring equipment should be re-installed
and surveyed to minimize data loss. We further recommend that the Road Commission
match existing culvert invert elevations on both ends of the new culvert to the existing
invert elevations as much as possible to ensure maintained fish passage through this man-
made structure.
If you have any questions regarding the information provided within this technical
memorandum, please do not hesitate to contact our office at (269) 344-7117
Site #1 (3 loggers) north of 4484 E. Cedar Lake Dr.
Site #2 (2 loggers) d k d
Jones
Lake Outflow
Site #2
3481 W. Cedar Lake Rd.
Site #3 (3 loggers)7588 Teal
Site #4 (1 logger)4840 E. Cedar Lake Dr.
Site #5 (1 logger)
Site #8 (1 logger)4884 Arron Dr.
Site #9 (1 logger)7448 Lakewood Dr.
Site #10 (1 logger)Site #5 (1 logger)6967 Lakewood Dr.
Site #6 (2 loggers)7906 W. Cedar Lake Rd.
Site #7 (2 loggers)4795 W. Cedar Lake Rd.
Site #10 (1 logger)7173 Huntington Dr.
Site #11 (1 logger)Lot north of 6933 Huntington Dr.
Lake Outflow (1 logger)
Site #1Site #7
Jones Creek (1 logger)
Sherman Creek (2 loggers)
King’s Corner (1 logger)
Sherman 2
Sherman 1
Site #4
Site #6
King’s Corner
Site #3
Sites 1-3 were original Phase I monitoring locations.
Sites 4-7 were added as part of Phase II
Site #9
Site #8
monitoring efforts.
Sites 8-11 were added as part of Augmentation Feasibility Study efforts.
Site #10
Site #11Site #5
FIGURE
1536 E. Michigan Ave., Suite 300, Kalamazoo, MI 49007 phone (269) 344-7117 fax (269) 344-2493
FIGURE Map of groundwater and surface water elevation monitoring sites located around the perimeter of Cedar Lake.
607.5
608
608.5
609
609.5
610
610.5
611
evat
ion
(ft)
Figure 2. 2016 Cedar Lake Groundwater /Surface Water Elevations (Site 1)
PZ-01d PZ-1S2 Lake Level PZ-1s
North Outlet Weirs Elevation = 608.64 (East Side)
603
603.5
604
604.5
605
605.5
606
606.5
607
3/1/16 3/31/16 4/30/16 5/30/16 6/29/16 7/29/16 8/28/16 9/27/16 10/27/16 11/26/16
El
Date/Time
607.0
607.5
608.0
608.5
609.0
609.5
610.0
610.5
611.0
Elev
atio
n (ft
)Figure 3. 2016 Cedar Lake Groundwater /Surface Water Elevations (Site 2)
Lake Level Pz-2d Pz-2s
North Outlet Weirs Elevation = 608.64 (East Side)
603.0
603.5
604.0
604.5
605.0
605.5
606.0
606.5
3/1/16 3/31/16 4/30/16 5/30/16 6/29/16 7/29/16 8/28/16 9/27/16 10/27/16 11/26/16
Date/Time
607.5
608.0
608.5
609.0
609.5
610.0
610.5
611.0
leva
tion
(ft)
Figure 4. 2016 Cedar Lake Groundwater /Surface Water Elevations (Site 3)
Lake Level PZ-3d PZ-3s PZ-3s2
North Outlet Weirs Elevation = 608.64 (East Side)
603.0
603.5
604.0
604.5
605.0
605.5
606.0
606.5
607.0
3/1/16 3/31/16 4/30/16 5/30/16 6/29/16 7/29/16 8/28/16 9/27/16 10/27/16 11/26/16
El
Date/Time
607.5
608.0
608.5
609.0
609.5
610.0
610.5
611.0
evat
ion
(ft)
Figure 5. 2016 Cedar Lake Groundwater /Surface Water Elevations (Site 4)
Lake Level PZ-04s
North Outlet Weirs Elevation = 608.64 (East Side)
603.0
603.5
604.0
604.5
605.0
605.5
606.0
606.5
607.0
3/1/16 3/31/16 4/30/16 5/30/16 6/29/16 7/29/16 8/28/16 9/27/16 10/27/16 11/26/16
El
Date/Time
607.5
608.0
608.5
609.0
609.5
610.0
610.5
611.0
evat
ion
(ft)
Figure 6. 2016 Cedar Lake Groundwater /Surface Water Elevations (Site 5)
Lake Level PZ-5s
North Outlet Weirs Elevation = 608.64 (East Side)
603.0
603.5
604.0
604.5
605.0
605.5
606.0
606.5
607.0
3/1/16 3/31/16 4/30/16 5/30/16 6/29/16 7/29/16 8/28/16 9/27/16 10/27/16 11/26/16
El
Date/Time
607.5
608.0
608.5
609.0
609.5
610.0
610.5
611.0
evat
ion
(ft)
Figure 7. 2016 Cedar Lake Groundwater /Surface Water Elevations (Site 6)
Lake Level PZ-6s2 PZ-6s
North Outlet Weirs Elevation = 608.64 (East Side)
603.0
603.5
604.0
604.5
605.0
605.5
606.0
606.5
607.0
3/1/16 3/31/16 4/30/16 5/30/16 6/29/16 7/29/16 8/28/16 9/27/16 10/27/16 11/26/16
El
Date/Time
608.0
608.5
609.0
609.5
610.0
610.5
611.0
611.5
612.0
evat
ion
(ft)
Figure 8. 2016 Cedar Lake Groundwater /Surface Water Elevations (Site 7)
Lake Level PZ-7s PZ-7s2
603.0
603.5
604.0
604.5
605.0
605.5
606.0
606.5
607.0
607.5
3/1/16 3/31/16 4/30/16 5/30/16 6/29/16 7/29/16 8/28/16 9/27/16 10/27/16 11/26/16
El
Date/Time
North Outlet Weirs Elevation = 608.64 (East Side)
603 5604.0604.5605.0605.5606.0606.5607.0607.5608.0608.5609.0609.5610.0610.5611.0
evat
ion
(ft)
Figure 9. 2016 Cedar Lake Groundwater /Surface Water Elevations (Site 8)
Lake Level PZ-8s
North Outlet Weirs Elevation = 608.64 (East Side)
595.0595.5596.0596.5597.0597.5598.0598.5599.0599.5600.0600.5601.0601.5602.0602.5603.0603.5
3/1/16 3/31/16 4/30/16 5/30/16 6/29/16 7/29/16 8/28/16 9/27/16 10/27/16 11/26/16
El
Date/Time
603 5604.0604.5605.0605.5606.0606.5607.0607.5608.0608.5609.0609.5610.0610.5611.0
evat
ion
(ft)
Figure 10. 2016 Cedar Lake Groundwater /Surface Water Elevations (Site 9)
Lake Level PZ-9s
North Outlet Weirs Elevation = 608.64 (East Side)
595.0595.5596.0596.5597.0597.5598.0598.5599.0599.5600.0600.5601.0601.5602.0602.5603.0603.5
3/1/16 3/31/16 4/30/16 5/30/16 6/29/16 7/29/16 8/28/16 9/27/16 10/27/16 11/26/16
El
Date/Time
603 5604.0604.5605.0605.5606.0606.5607.0607.5608.0608.5609.0609.5610.0610.5611.0
evat
ion
(ft)
Figure 11. 2016 Cedar Lake Groundwater /Surface Water Elevations (Site 10)
Lake Level PZ-10s
North Outlet Weirs Elevation = 608.64 (East Side)
595.0595.5596.0596.5597.0597.5598.0598.5599.0599.5600.0600.5601.0601.5602.0602.5603.0603.5
3/1/16 3/31/16 4/30/16 5/30/16 6/29/16 7/29/16 8/28/16 9/27/16 10/27/16 11/26/16
El
Date/Time
603 5604.0604.5605.0605.5606.0606.5607.0607.5608.0608.5609.0609.5610.0610.5611.0
evat
ion
(ft)
Figure 12. 2016 Cedar Lake Groundwater /Surface Water Elevations (Site 11)
Lake Level PZ-11s
North Outlet Weirs Elevation = 608.64 (East Side)
595.0595.5596.0596.5597.0597.5598.0598.5599.0599.5600.0600.5601.0601.5602.0602.5603.0603.5
3/1/16 3/31/16 4/30/16 5/30/16 6/29/16 7/29/16 8/28/16 9/27/16 10/27/16 11/26/16
El
Date/Time
12.4313.15 13.48
10.94
15.16 14.88
15.97
16.89
13.96 14.14
10 94
12.18
15.00
20.00
ches
)
Figure 13. Summer (Jun - Sept) Precipitation Totals for Cedar Lake(Precipitation Source: Harrisville, MI, CO-OP Station #203628,
Alcona County Cedar Lake Rain Gauge,Oscoda, MI Oscoda Wurtsmith Airport Station #14808, Iosco County)
precipitation
June-September Precipitation Threshold = 11.0 inches per summer (336 Mgal on Cedar Lake) to avoid >3-inch lake level drop
9.99 10.08
7.61
N/A
7.768.61
10.3510.94
0.00
5.00
10.00
1998 1999 2000 2001 2002 2003 2004 2005 2006 2007 2008 2009 2010 2011 2012 2013 2014 2015 2016
Sum
mer
Tot
al (i
nc
Date
2.00
2.50
3.00
608.5
609.0
609.5
610.0
610.5
ecip
itatio
n (i
n)
Elev
atio
n (ft
)Figure 14. 2016 Cedar Lake Water Elevelation and Measured Rainfall
Lake Level Precip
North Outlet Weirs Elevation = 608.64 (East Side)
0.00
0.50
1.00
1.50
606.0
606.5
607.0
607.5
608.0
PreE
Date/Time
6065707580859095
100105110115120125
ed F
low
(cfs
)Figure 15. 2016 Estimated Jones Creek Flows
Jones Creek
05
1015202530354045505560
3/1/16 3/31/16 4/30/16 5/30/16 6/29/16 7/29/16 8/28/16 9/27/16 10/27/16 11/26/16
Estim
ate
Date/Time
6065707580859095
100105110115120125
ed F
low
(cfs
)Figure 16. 2016 Estimated Sherman Creek Flows
Sherman Creek
05
1015202530354045505560
3/1/2016 3/31/2016 4/30/2016 5/30/2016 6/29/2016 7/29/2016 8/28/2016 9/27/2016 10/27/2016 11/26/2016
Estim
ate
Date/Time
6065707580859095
100105110115120125
ed F
low
(cfs
)Figure 17. 2016 Estimated Cedar Lake Outflows
Lake outflow
05
1015202530354045505560
3/1/16 3/31/16 4/30/16 5/30/16 6/29/16 7/29/16 8/28/16 9/27/16 10/27/16 11/26/16
Estim
ate
Date/Time
6065707580859095
100105110115120125
ed F
low
(cfs
)Figure 18. 2016 Estimated Kings Corner Flows
Kings Corner
05
1015202530354045505560
3/1/16 3/31/16 4/30/16 5/30/16 6/29/16 7/29/16 8/28/16 9/27/16 10/27/16 11/26/16
Estim
ate
Date/Time
6065707580859095
100105110115120125
ed F
low
(cfs
)Figure 19. 2016 Estimated Cedar Lake Inflows/Outflows
Lake outflow Sherman Creek Jones Creek Kings Corner
3/21/16 to 7/22/16 Sherman Creek = 922 MGal (Inflow)Jones Creek = 648 Mgal (Inflow)Kings Corner = 185 MGal (Outflow)Cedar Lake Outflow = 2,621 MGal (Outflow)
Over 123 days (3/21/16 to 7/22/16)Max. Lake Outflow:
121.06 cfs(April 6, 2016)
05
1015202530354045505560
3/1/16 3/31/16 4/30/16 5/30/16 6/29/16 7/29/16 8/28/16 9/27/16 10/27/16 11/26/16
Estim
ate
Date/Time
15
20
25
ed F
low
(cfs
)Figure 20. 2016 Estimated Kings Corner Total Outflow Losses
Kings
3/21/16 to 11/18/16
Kings Corner = 216 MGal (Outflow)
Over 243 days (3/21/16 to 11/18/16)
Note: This volume reflects "lost inflow" to Cedar Lake.
0
5
10
3/1/16 3/31/16 4/30/16 5/30/16 6/29/16 7/29/16 8/28/16 9/27/16 10/27/16 11/26/16
Estim
ate
Date/Time
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