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State of the Lakes Report

Warner Beach_-6

2023 State of the Lakes

2023 SOTL Cover

The State of the Lakes provides an annual health synopsis of Greater Madison’s five Yahara lakes (Mendota, Monona, Wingra, Waubesa, and Kegonsa). The chain of lakes and the land areas that drain to them are shown in Figure 1. Focusing on major drivers and indicators of water quality collected over the prior year (2023), the analysis summarizes lake and watershed health factors, trends, and the likely causes of observed conditions. The report begins with lake-specific health dashboards before reviewing five areas of watershed impact and lake response.

Authored by Clean Lakes Alliance Deputy Director and Chief Science Officer Paul Dearlove, this report is a product of collaboration involving multiple government and scientific contributors. We are grateful to the following entities and information sources: U.S. Geological Survey, University of Wisconsin-Madison, Wisconsin Department of Natural Resources, Wisconsin Salt Wise, Public Health Madison & Dane County, Dane County Land & Water Resources Department, and
Clean Lakes Alliance’s volunteer LakeForecast monitors.

Lakes_Watersheds_Agriculture-map

Figure 1: Yahara lakes watershed showing land areas that drain directly to each lake. Yellow denotes agricultural areas that comprise most of the 384-square-mile watershed.

2023 key takeaways

  • Drought conditions limited runoff and phosphorus delivery to the lakes, helping all five lakes attain “good” to “excellent” rankings for phosphorus levels and “good” rankings for water clarity.
  • LakeForecast monitors observed comparatively fewer nearshore cyanobacteria (blue-green algae) blooms compared to prior years.
  • Historically rising chloride concentrations caused by winter salting is an ongoing water quality concern, with the highest levels measured in Lake Wingra.
  • Per- and polyfluoroalkyl substances (PFAS) are an emerging contaminant of concern, with lakes Monona, Waubesa, and Kegonsa recently listed as federally impaired for these forever chemicals.
  • Progress continues around the adoption of phosphorus-reducing land conservation practices, but more action is needed to reach and sustain water quality goals, including getting 100% of agricultural acres covered by nutrient management plans and developing more manure management facilities.

Lake Mendota

Lake Mendota

Lake Type: Drainage
Direct Drainage Area:
217 sq. miles
Total Drainage Area:
232.4 sq. miles
Surface Area:
9,847 acres
Shoreline Length:
22 miles
Mean Depth: 42 feet
Maximum Depth:
83 feet
Volume:
133,407 million gallons
Flushing Rate:
22% of volume/year

Lake Mendota sits at the top of the chain and is the largest of the five Yahara lakes by surface area, depth, and volume. Its direct drainage area consists predominantly of agricultural land uses. Inlet tributaries include Pheasant Branch Creek (west shore); and Sixmile Creek, Dorn Creek, Token Creek, and the Yahara River (north shore). The lake’s outlet (southeast shore) directs overflow water through the Yahara River and into Lake Monona. It has been listed as federally impaired for phosphorus since 2011.

Lake Mendota Health Dashboard

Lake Mendota Health Dashboard 2023

Lake Monona

Lake Monona

Lake Type: Drainage
Direct Drainage Area:
40.5 sq. miles
Total Drainage Area:
278 sq. miles
Surface Area:
3,277 acres
Shoreline Length:
13 milesMean Depth: 27 feet
Maximum Depth:
74 feet
Volume:
29,059 million gallons
Flushing Rate:
91% of volume/year

Lake Monona is the second largest of the five Yahara lakes by surface area, depth, and volume. It sits immediately downstream of Lake Mendota in the upper half of the chain. The lake’s direct drainage area consists mostly of urban land uses. Inlet tributaries flowing into the lake include Murphy’s (Wingra) Creek (west shore); the Yahara River (north shore); and Starkweather Creek (northeast shore). The lake’s outlet (south shore) directs overflow water through the Yahara River and into Upper Mud Lake and Lake Waubesa. It has been listed as federally impaired for PCBs since 1998, phosphorus since 2011, and PFAS since 2022.

Lake Monona Health Dashboard

Lake Monona Health Dashboard 2023

Lake Wingra

Lake Wingra

Lake Type: Drainage
Direct Drainage Area:
5.4 sq. miles
Total Drainage Area:
5.4 sq. miles
Surface Area:
321 acres
Shoreline Length:
3.7 miles
Mean Depth: 9 feet
Maximum Depth:
14 feet
Volume:
1,585 million gallons
Flushing Rate:
77% of volume/year

Lake Wingra is the smallest of the five major lakes by surface area, depth, and volume. Originally a deep-water marsh, this dredged waterbody now flows into Lake Monona via Murphy’s (Wingra) Creek. The lake’s direct drainage area is located entirely within the city of Madison and dominated by urban land uses. Three minor, unnamed inlet tributaries flow into the lake at points along its west and southwest shore. It has been listed as federally impaired for phosphorus since 2011 and PCBs since 2012.

Lake Wingra Health Dashboard

Lake Wingra Health Dashboard 2023

Lake Waubesa

Lake Waubesa

Lake Type: Drainage
Direct Drainage Area:
43.6 sq. miles
Total Drainage Area:
325 sq. miles
Surface Area:
2,083 acres
Shoreline Length:
9.4 miles
Mean Depth: 15 feet
Maximum Depth:
38 feet
Volume:
10,567 million gallons
Flushing Rate:
320% of volume/year

Lake Waubesa is the fourth largest of the Yahara lakes by surface area and volume. It sits immediately downstream of Upper Mud Lake and Lake Monona in the lower half of the chain. The lake’s direct drainage area is represented by a mix of urban and rural/agricultural land uses. Inlet tributaries that drain into the lake include Nine Springs Creek and Penitto Creek (flowing into Upper Mud Lake to the north); the Yahara River (north shore); as well as Swan Creek and Murphy’s Creek (southwest shore). The lake’s outlet (east shore) directs overflow water through the Yahara River and into Lake Kegonsa. It has been listed as federally impaired for phosphorus since 2011 and PFAS since 2022.

Lake Waubesa Health Dashboard

Lake Waubesa Health Dashboard 2023

Lake Kegonsa

Lake Kegonsa

Lake Type: Drainage
Direct Drainage Area:
54.4 sq. miles
Total Drainage Area:
384.6 sq. miles
Surface Area:
3,210 acres
Shoreline Length:
9.6 miles
Mean Depth: 17 feet
Maximum Depth:
32 feet
Volume:
17,700 million gallons
Flushing Rate:
220% of volume/year

Lake Kegonsa is the third largest of the Yahara lakes by surface area and volume. It sits immediately downstream of Lake Waubesa and Lower Mud Lake in the lower half of the chain. The lake’s direct drainage area consists predominantly of rural/agricultural land uses. Inlet tributaries that drain into the lake include Door Creek (north shore) and two unnamed creeks (southwest and northeast shore). The lake’s outlet (east shore) directs overflow water through the Yahara River toward the Rock and Mississippi Rivers. It has been listed as federally impaired for phosphorus since 2011 and PFAS since 2022.

Lake Kegonsa Health Dashboard 2023

Watershed health indicators

The State of the Lakes assesses five areas of interest that represent vital, interconnected pieces of the larger water quality puzzle. These areas of analysis, illustrated in Figure 2, include both outputs (i.e., land-use actions taken) and outcomes (i.e., measured water quality responses). They were chosen to illustrate critical cause-and-effect principles that play out as water gets funneled through the watershed. 

Watershed example - Figure 2

Figure 2: Cross-section illustration of an example watershed showing five areas of analysis. Example scoring dials represent condition status and trend for each area of analysis.

Phosphorus availability and transport are central themes in this analysis given the nutrient’s dominant role in affecting overall lake conditions. Although a natural element essential for plant and animal growth, it can easily harm water quality due to overuse and poor management. Common sources of phosphorus pollution include eroded soil, fertilizer runoff, autumn leaf debris left in city streets, poorly managed livestock manure, sewage releases, and uncollected pet waste. It is estimated that one pound of phosphorus can generate up to 500 pounds of algae growth in our lakes.

1. Weather and climate drivers

Dials 1 - Weather and Climate Drivers - 2023

Regardless of whether it’s changes in temperature, precipitation, ice cover, or some other factor, lakes dynamically respond to their environment. Regional heating and cooling patterns influence what types of aquatic organisms can thrive, how and when a lake mixes, and the timing and magnitude of annual freeze cycles. Meanwhile, the timing, intensity, and amount of rainfall falling over the watershed determine what can get moved from the land surface into our waters, including phosphorus-containing materials that fuel algal growth and turn the lakes green.  

Winter Season

Winter ice conditions and the timing of ice-off influence everything from water temperatures to the reproductive success of aquatic life. Ice quality and overlying snow depth affect how much sunlight can penetrate to warm the water column and facilitate dissolved oxygen production through photosynthesis. Research by Dr. Zachary Feiner at UW-Madison’s Center for Limnology documents the impacts of early ice-off. As ice-off dates move earlier due to climate change, algae production gets an early start and then collapses right when the daphnia (a type of zooplankton) hatch and are looking for food. This means less zooplankton to eat by juvenile fish and less grazing of algae. Resulting impacts can range from poorer walleye recruitment to more intense algal blooms. 

In 2023, Lake Mendota remained frozen for 98 days (12/25/22 – 4/2/23), or 13 days longer than in 2022. This is on par with its median ice-cover duration of 102 days as measured over the last 168 seasons. Historical evidence shows ice-cover durations in decline, with Mendota having lost about a month of ice cover on average since recordkeeping began.

Lake Monona in March 2023, courtesy Robert Bertera
Lake Monona in March 2023, courtesy Robert Bertera

Shorter and warmer winters lead to warmer lake temperatures earlier in the year, effectively creating a longer growing season for algae and aquatic plants. Warmer winters can also contribute to greater runoff and phosphorus delivery when wet precipitation falls on frozen soils. Rather than soak into the ground, rainfall more easily turns into runoff that can carry land-spread manure and other contaminants into the ditches and streams that drain to the lakes. It is estimated that, on average, nearly half of the total phosphorus loading through Lake Mendota’s monitored stream tributaries occurs from January to March, making late winter and early spring a vulnerable time for our lakes.

Warmer Growing Season

The meteorological summer of 2023 (June 1-August 31) was Wisconsin’s sixth driest on record. Less rainfall leads to less stormwater runoff, meaning less phosphorus washing into our lakes. Based on weather data collected at the Dane County Regional Airport in Madison, the watershed transitioned from a three-year period of above-normal rainfall to a three-year period of below-normal rainfall.

Inches of Rainfall 2023-2024

May and June’s collective rainfall totaled only 2.01 inches, compared to the normal 9.38 inches, with only one day receiving 0.50-inch or greater rainfall. The second half of the summer remained dry with July and August collectively experiencing only three days of 0.50-inch or greater rainfall. While July’s 6.21 inches surpassed the monthly normal (4.51 inches), drought conditions persisted with August receiving lower-than-normal rainfall (2.42 inches), further contributing to the already low lake levels. With 2023 capping a three-year period of below-normal rainfall, the impacts of reduced runoff were evident in lower phosphorus delivery (called “loading”) and positive water-clarity responses in all five lakes.

2. Watershed phosphorus mass balance

Dials 2 - Watershed Phosphorus Mass Balance - 2023

Calculating the difference between the mass of phosphorus entering (imported into) and leaving (exported from) the watershed tells us whether the net balance is trending in the right direction. The movement and fate of livestock, feed, fertilizer, harvested crops, animal waste, and other phosphorus sources are factored into the analysis. The goal is to attain a negative balance, indicating more phosphorus is being exported than imported on an annual basis. This situation reduces the overall availability of phosphorus from being able to reach area waterways. 

Conversely, a positive balance signals an annual net accumulation of phosphorus in the watershed, usually leading to its gradual buildup in area soils. Phosphorus-saturated soils that are subject to erosion and not protected by year-round plant cover can eventually end up at the bottom of nearby lakes and streams. Phosphorus is also more easily “leached” (or released in dissolved form) from these soils when they encounter rainwater and snowmelt. 

Past improvements to the overall mass balance are attributed to multiple factors. They include decreases in imported commercial fertilizer, less phosphorus-containing feed supplements consumed by livestock, exported byproducts of manure treatment, and advanced phosphorus-management strategies implemented by Madison Metropolitan Sewerage District (among others). Examples of mass balance detractors include increases in livestock numbers and milk production.

3. Land conservation practices

Dials 3 - Land Conservation Practices - 2023

The adoption of land conservation practices helps minimize the amount of runoff and soil erosion that harms water quality. Examples include preserving and increasing perennial grasslands and natural vegetation, establishing permanent vegetation, maintaining protective cover crops on harvested farm fields, raising livestock on rotationally grazed pastures, and removing fall leaf litter from city streets. In addition, the use of nutrient management plans helps agricultural producers better understand how operational decisions can maximize soil health and productivity while limiting erosion and phosphorus runoff.

Yahara River downstream of Lake Kegonsa, courtesy Robert Bertera
Yahara River downstream of Lake Kegonsa, courtesy Robert Bertera

In accordance with state law, nutrient management plans are required on all farms to serve as nutrient-accounting tools, ensuring that manure and fertilizer applications meet crop needs while limiting runoff risks.  Based on the latest landowner records filed with Dane County Land & Water Resources (Figure 3), 44,387 out of 84,321 total agricultural acres in the Yahara lakes watershed (53%) were mapped as having a nutrient management plan in 2023 – a 36% increase over just the last seven years. These numbers are believed to be an underrepresentation of the total amount of watershed acres under nutrient management planning since not every plan is recorded with Dane County. Achieving 100% compliance will be a big step forward in attaining related phosphorus reductions that come with sound planning.

Figure 3:  Farmland acres in the Yahara lakes watershed that have a nutrient management plan filed with Dane County. Data credit: Kyle Minks, Dane County Land & Water Resources.
Figure 3: Farmland acres in the Yahara lakes watershed that have a nutrient management plan filed with Dane County. Data credit: Kyle Minks, Dane County Land & Water Resources.

Currently, available soil-test information from farmland in the upper half of the watershed has a Rotational Average Phosphorus Index (PI) of 2.8, representing estimated pounds of phosphorus loss per acre per year. The Phosphorus Index is a tool used to assess the potential of phosphorus to move from agricultural fields to surface water, with higher numbers representing greater risk. According to modeling summarized in RENEW THE BLUE: A Community Guide for Cleaner Lakes & Beaches in the Yahara Watershed (2022), a Rotational Average PI of 2.1 or less is needed to reach phosphorus-loading targets and water quality goals in the Yahara lakes. Since 2016, values in the upper watershed north of Lake Mendota have averaged between 2.3 and 3.3. State standards require all fields covered by a Nutrient Management Plan to have a Rotational Average PI of 6 or less.

4. Phosphorus delivery to the lakes

Dials 4 - Phosphorus Delivery to the Lakes - 2023

Most phosphorus is delivered to the Yahara chain of lakes through tributary streams that collect and channel upland-generated runoff as it moves downhill. How much is transported depends on the seasonal timing and intensity of runoff events, the location and availability of major phosphorus sources, and measures taken to contain those sources and manage runoff. Over the course of an average year within the past decade, approximately 40% of the total phosphorus load occurred during the months of January, February, and March.

Pheasant Branch Creek flowing into the west side of Lake Mendota, courtesy Robert Bertera
Pheasant Branch Creek flowing into the west side of Lake Mendota, courtesy Robert Bertera

Stream monitoring is used as a tool to evaluate the effectiveness of conservation practices by tracking phosphorus loading. Loading describes the total mass of phosphorus delivered to a specific location in a stream over time. In our case, we characterize loading in pounds of phosphorus (calculated by multiplying in-stream concentrations by streamflow) delivered through Lake Mendota’s monitored stream tributaries in a given “water year” (Oct. 1 – Sep. 30). Perched at the top of the chain and receiving most of the drainage from the Yahara lakes watershed, the condition of Lake Mendota offers a good indicator for how the downstream lakes will be impacted. Lake Mendota is also the largest lake with the greatest number of monitored streams and the most complete long-term dataset. Most of the phosphorus received by the lower lakes in the chain is through the outlets of the upper lakes as it cascades through the system.

Figure 4: Phosphorus loading through Lake Mendota’s monitored stream tributaries in relation to total precipitation. Phosphorus loading data credit: U.S. Geological Survey. Precipitation data credit: NOAA Regional Climate Center, Dane County Regional Airport.
Figure 4: Phosphorus loading through Lake Mendota’s monitored stream tributaries in relation to total precipitation. Phosphorus loading data credit: U.S. Geological Survey. Precipitation data credit: NOAA Regional Climate Center, Dane County Regional Airport.

Figure 4 shows the change in stream-monitored phosphorus loading since 2013. Total precipitation is also plotted in orange to distinguish between wet and dry years. From 2021-2023, average annual phosphorus loading to Lake Mendota significantly declined and has even dipped slightly below target levels. This was largely due to drier weather after years of above-average precipitation, reducing the amount of runoff transporting phosphorus to the lakes. Scientists estimate a doubling of summer days when the lakes are clear and free of algal blooms if these lower levels can be maintained.

5. In-lake water quality responses

Dials 5 - In-Lake Water Quality Responses - 2023

Several in-lake metrics are used to assess overall lake health and track changes over time. Those metrics include water clarity, phosphorus concentration, presence of cyanobacteria (blue-green algae) blooms, and beach closures. Each is summarized in the following figures. All five lakes fared relatively well in 2023 based on these specific health indicators, ranking good to excellent for phosphorus and good for clarity.

Phosphorus

In-lake phosphorus concentrations for all five lakes were comparatively low relative to the prior 10 years, but without any obvious trends over this period (Figure 5). Even when looking at longer time horizons, trends are difficult to identify. When averaged across individual decades beginning in the 1980s, lakes Monona and Waubesa show slight downward trends while those for lakes Mendota and Kegonsa are not evident. This speaks to the reality that more work is needed to reduce phosphorus loading if we hope to improve upon prevailing trends.

Figure 5:  Median summer (Jul-Aug) phosphorus concentrations and corresponding water quality classifications by lake type.
Notes: Phosphorus sampling was not performed in lakes Kegonsa, Waubesa, and Wingra in 2020, and in lakes Kegonsa and Waubesa in 2021. Water quality classifications based on Wisconsin Department of Natural Resources’ criteria. Data credit: Richard Lathrop, UW-Madison Center for Limnology.
Figure 5: Median summer (Jul-Aug) phosphorus concentrations and corresponding water quality classifications by lake type. Notes: Phosphorus sampling was not performed in lakes Kegonsa, Waubesa, and Wingra in 2020, and in lakes Kegonsa and Waubesa in 2021. Water quality classifications based on Wisconsin Department of Natural Resources’ criteria. Data credit: Richard Lathrop, UW-Madison Center for Limnology.
Figure 5:  Median summer (Jul-Aug) phosphorus concentrations and corresponding water quality classifications by lake type.
Notes: Phosphorus sampling was not performed in lakes Kegonsa, Waubesa, and Wingra in 2020, and in lakes Kegonsa and Waubesa in 2021. Water quality classifications based on Wisconsin Department of Natural Resources’ criteria. Data credit: Richard Lathrop, UW-Madison Center for Limnology.

Recent drought years that limit phosphorus delivery because of reduced runoff loadings entering the lakes continue to have a positive effect on in-lake phosphorus concentrations. Lake Mendota’s concentrations after fall turnover hit a new record low in 2023 (Figure 6) following three years of relatively low external phosphorus loadings from the surrounding watershed. Turnover occurs when deeper lakes cool to the point where the water column can completely mix. Higher phosphorus concentrations that have built up throughout the summer in the bottom waters are then mixed throughout the lake. As less phosphorus enters the lake from the watershed, this bottom-water buildup of phosphorus is reduced, thereby reducing internal (in-lake) sources that can fuel algal growth the following year. 

Figure 6: Lake Mendota total phosphorus concentrations at fall turnover measured at the lake surface. Credit: Richard Lathrop, UW-Madison Center for Limnology.
Figure 6: Lake Mendota total phosphorus concentrations at fall turnover measured at the lake surface.
Credit: Richard Lathrop, UW-Madison Center for Limnology.

Fall turnover phosphorus concentrations were also low in 1988 and 2012 following those extended droughts. This shows that Lake Mendota’s phosphorus levels decline when loading from the watershed is reduced. Similar responses occurred following the wet, high-loading years of 2008 and 2018-19 when fall turnover phosphorus concentrations were very high. Soon after these years, Lake Mendota’s phosphorus status quickly dropped back to more average levels. This is another sign that reduced external loadings from the surrounding watershed can result in significant and relatively quick water quality improvements.

Boating on Lake Waubesa, courtesy Robert Bertera
Boating on Lake Waubesa, courtesy Robert Bertera

Water Clarity

Offshore water clarity for all five lakes was comparatively high relative to the prior 10 years, with median summer values generally trending higher over this period (Figure 7). However, when looking at longer time horizons, trends are more mixed. When averaged across individual decades beginning in the 1980s, lakes Mendota and Waubesa show slight downward trends while those for lakes Monona and Kegonsa are not discernible.

Figure 7:  Median summer (Jul-Aug) offshore water clarity readings and corresponding water quality classifications by lake type.
Notes: Water clarity information was not available for lakes Monona and Wingra in 2020. Water quality classifications based on Wisconsin Department of Natural Resources’ criteria. Data credit: Richard Lathrop, UW-Madison Center for Limnology.
Figure 7: Median summer (Jul-Aug) offshore water clarity readings and corresponding water quality classifications by lake type. Notes: Water clarity information was not available for lakes Monona and Wingra in 2020. Water quality classifications based on Wisconsin Department of Natural Resources’ criteria. Data credit: Richard Lathrop, UW-Madison Center for Limnology.
Figure 7:  Median summer (Jul-Aug) offshore water clarity readings and corresponding water quality classifications by lake type.
Notes: Water clarity information was not available for lakes Monona and Wingra in 2020. Water quality classifications based on Wisconsin Department of Natural Resources’ criteria. Data credit: Richard Lathrop, UW-Madison Center for Limnology.

Because water clarity often varies across a given lake, Clean Lakes Alliance uses a network of trained volunteer monitors to collect additional data through its LakeForecast program. From Memorial Day through Labor Day, monitors submit at least twice-weekly reports on water clarity, water temperature, and the severity of floating green algae and cyanobacteria blooms (among other variables). This information can be seen in near-real-time on LakeForecast.org and the free LakeForecast app, allowing the public to stay up to date on current lake conditions. These reports are also used to raise awareness about changing water quality conditions, advocate for improvement projects, and inform this annual State of the Lakes.

Figure 8: LakeForecast monitor locations
Figure 8: LakeForecast monitor locations

To measure nearshore clarity, monitors use a sampling device called a turbidity tube to report conditions at nearly 90 sites spread around all five lakes (Figure 8). Figure 9 shows the median summer (Jul-Aug) clarity readings for each lake from 2014-2023. Values under 50 as measured on the 120-cm device are considered “murky,” between 50-80 “fair,” and between 80-120 “good.” Consistent with offshore clarity readings using a Secchi disk, most values for 2023 fell within the good range, except for Lake Mendota which was at the upper range of fair.

Figure 9:  Median summer (Jul-Aug) nearshore clarity readings for each lake (2014-2023).
Figure 9: Median summer (Jul-Aug) nearshore clarity readings for each lake (2014-2023).

Cyanobacteria Blooms

To determine cyanobacteria bloom frequency, the number of days on each lake with at least one report of a strong cyanobacteria bloom observed within the individual monitoring sites was counted. By dividing the number of “cyanobacteria bloom days” by the total number of sampling days for each lake, a percentage is generated representing how often the monitors observed at least one major bloom within their sampling area. This method lessens overreporting in situations when different monitors report the same cyanobacteria bloom.

Figure 10:  Percent of sampling days (Jun-Aug) when strong evidence of a cyanobacteria bloom was observed at one or more sites on each lake.
Figure 10: Percent of sampling days (Jun-Aug) when strong evidence of a cyanobacteria bloom was observed at one or more sites on each lake.

Figure 10 shows the percentage of sampling days when strong evidence of a cyanobacteria bloom was observed on each lake (2014-2023). Overall, monitors reported comparatively low cyanobacteria blooms during the 2023 sampling period (Jun-Aug), with most of the significant blooms occurring early in the season. Monitors on lakes Monona, Waubesa, and Kegonsa did not report a single significant bloom. This is welcome news after 2022’s record-high bloom count on Lake Kegonsa. Lake Wingra experienced similar bloom counts to 2022, and Lake Mendota had a handful of significant blooms reported in 2023 after not experiencing any in 2022.

Clean Lakes Alliance volunteer removes aquatic plant debris from Spring Harbor Beach in September 2023
Clean Lakes Alliance volunteer removes aquatic plant debris from Spring Harbor Beach in September 2023

Beach Closures

Beach closures are another useful indicator of general lake health. Clean Lakes Alliance looks at closure data provided by Public Health Madison & Dane County for 17 beaches (Figure 11). Covering four of the five Yahara lakes, these tested public beaches were selected due to the consistency of tracking data over the prior 10-year period. Results are reported as total closure days recorded for each season, roughly running from Memorial Day to Labor Day. For example, if two beaches on a given lake are closed for a total of five days each, 10 closure days would be reported for that lake.

Figure 11:  Beach closure days by lake. Includes beaches consistently monitored since 2013. Lake Mendota: Governor Nelson, Warner, Mendota County, James Madison, Memorial Union Pier, Marshall, Tenney, and Spring Harbor; Lake Monona: B.B. Clarke, Bernie's, Brittingham, Esther, Hudson, Olbrich, Olin; Lake Wingra: Vilas; Lake Waubesa: Goodland County; Lake Kegonsa: None. Data credit: Public Health Madison & Dane County.
Figure 11: Beach closure days by lake. Includes beaches consistently monitored since 2013. Lake Mendota: Governor Nelson, Warner, Mendota County, James Madison, Memorial Union Pier, Marshall, Tenney, and Spring Harbor; Lake Monona: B.B. Clarke, Bernie’s, Brittingham, Esther, Hudson, Olbrich, Olin; Lake Wingra: Vilas; Lake Waubesa: Goodland County; Lake Kegonsa: None. Data credit: Public Health Madison & Dane County.

Closures are most often the result of high cyanobacteria and/or E. coli bacteria levels, with closure rates strongly influenced by timing and frequency of testing. Most beaches are tested once per week and then daily for beaches with a closure in effect. Cyanobacteria blooms, which are generally a product of high lake fertility, can be dangerous due to their potential to release toxins that can harm people, pets, and wildlife. High E. coli bacteria concentrations can also be harmful as they are an indicator of human or animal fecal matter in the water that may contain dangerous pathogens. In 2023, there were 82 beach-closure days reported, which is below both the long-term median and the 92 closures reported in 2022. Closures were relatively split between cyanobacteria and E. coli as the causes.

Growing Stewardship

Clean Lakes Alliance remains committed to fulfilling its vision of making Greater Madison renowned for its healthy lakes, lands, and waters. We do this through our daily mission to champion the lakes and watershed stewardship for the benefit of all. We are also proud to have assembled and led the 19-member partnership coalition, called the Yahara CLEAN Compact, that signed off on an updated lake-cleanup plan. RENEW THE BLUE: A Community Guide for Cleaner Lakes & Beaches in the Yahara Watershed (2022) reaffirmed goals and is now guiding action across multiple stakeholder groups.

Achieving and sustaining healthier local lakes is entirely possible. Increased awareness, involvement, and progress on needed project action are helping to move us in that direction. But more work and investment are clearly needed, and it will take all watershed stakeholders playing an active role to get us there. To learn more about the lakes and what you can do to help, visit cleanlakesalliance.org/renew-the-blue.

Clear water in November 2023 allows a view of the sandy bottom of Lake Monona near Turville Point
Photo courtesy Robert Bertera
Clear water in November 2023 allows a view of the sandy bottom of Lake Monona near Turville Point Photo courtesy Robert Bertera

About the State of the Lakes

The annual State of the Lakes is released each year as part of the Greater Madison Lake Guide. In it, we report out to the community on the state of water quality in our lakes. The report also looks at our collective progress toward our phosphorus reduction goal.

The report highlights information from many partners to share the most up-to-date science on water quality in our lakes. We feature local projects, including work in urban areas to protect stormwater quality and progress on farms to keep nutrients on the fields and out of our lakes.

In addition, we provide more information about Clean Lakes Alliance and our efforts to engage the community and advocate for the lakes. This report serves as a reference and a resource, highlighting community progress toward cleaner, healthier lakes for all.

Learn more about our lakes

Learn more about lakes Mendota, Monona, Wingra, Waubesa, and Kegonsa.

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