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HomeMy WebLinkAboutMemo - Mail Packet - 7/21/2020 - Memorandum From Jared Heath Re: 2020 Spring Water Quality Update - Upper Cache La Poudre WatershedUtilities electric · stormwater · wastewater · water PO Box 580 Fort Collins, CO 80522 970.212.2900 V/TDD: Dial 711 for Relay Colorado utilities@fcgov.com fcgov.com/utilities M E M O R A N D U M DATE: July 14, 2020 TO: Mayor Troxell and Councilmembers FROM: Jared Heath, Watershed Specialist THROUGH: Darin Atteberry, City Manager Theresa Connor, Interim Utilities Executive Director RE: 2020 Spring Water Quality Update – Upper Cache la Poudre Watershed Bottom Line: In the shared interest of monitoring the Upper Cache la Poudre (CLP) River drinking water supply, the City of Fort Collins, the City of Greeley, and the Tri-Districts partnered in 2008 to implement the Upper CLP Collaborative Watershed Monitoring Program. The goal of this monitoring effort is to assist the participants in meeting current and future drinking water treatment goals by reporting current water quality conditions and trends within the Upper CLP watershed. The attached water quality update provides a summary of temperature, snowpack, streamflow, and water quality conditions monitored in the Upper CLP watershed during the spring months of April and May in 2020. Background: The seasonal water quality updates are designed to inform the Upper CLP Watershed Collaborative Monitoring Program partners, their customers, and other community stakeholders about the condition of our source watershed and the quality of the raw drinking water supply. This seasonal reporting effort began in 2015 to provide a succinct and timely summary of current-year conditions in the Upper CLP Watershed. Seasonal updates are published for the spring, summer, and fall seasons. In depth water quality reporting is done through annual and five-year technical reports. All water quality reports and seasonal updates are made publicly available on the Fort Collins Utilities website, fcgov.com /source-water-monitoring. Spring 2020 Highlights: The Upper CLP watershed continues to be a reliable, high quality drinking water source for the City of Fort Collins. Snowpack conditions were slightly above normal by the end of the 2020 snow accumulation season. Peak snow water equivalent measuring 116 percent of normal for the CLP watershed. Over the spring season, dry and warm conditions were observed with below average precipitation and warmer than average air temperatures measured from March through DocuSign Envelope ID: A197C63C-385D-42DB-97DD-4FEEEB336D55 April. Despite these conditions, all water quality indicators at key sites along the Upper CLP River measured within the range of baseline conditions indicating normal water quality conditions on the Poudre River during the spring 2020 snowmelt runoff season. CC: Carol Webb, Utilities Deputy Director - Water Resources and Treatment Operations Jill Oropeza, Water Quality Services Director, Utilities Richard Thorp, Watershed Program Manager, Utilities DocuSign Envelope ID: A197C63C-385D-42DB-97DD-4FEEEB336D55 fcgov.com/water-quality SOURCE WATER MONITORING JWC - Joe Wright Creek above the confluence with the Poudre River PJW - Poudre River above the confluence with Joe Wright Creek PBR - Poudre River below the Town of Rustic PSF - Poudre River below the confluence with the Little South Fork PNF - Poudre River above the confluence with the North Fork at the City of Fort Collins’ Intake PBD - Poudre River below the confluence with the North Fork at the Bellvue Diversion The Upper Cache la Poudre (UCLP) Watershed Collaborative Monitoring Program was established in 2008 between the City of Fort Collins, the City of Greeley and Soldier Canyon Water Authority, to help meet present and future drinking water treatment goals. Water quality monitoring of our raw, Cache la Poudre River drinking water supply is conducted from April through November. Monitoring sites are strategically located throughout the UCLP. Water quality data provide valuable information about the health of our source watershed and raw water supply. The Spring 2020 Water Quality Update provides a seasonal summary of watershed conditions in the UCLP watershed by highlighting snowpack and streamflow conditions, as well as water quality information collected over the months of April and May. Water quality during spring snowmelt runoff is highly variable. To better capture this seasonal variability, monitoring is conducted two times per month from April through June. In 2020, the UCLP monitoring plan was adjusted to meet resource constraints because of the COVID-19 pandemic. For the Spring 2020 Water Quality Update, results are only reported for the two key monitoring sites located near the City of Fort Collins’ (PNF) and City of Greeley’s (PBD) water supply intake structures (Figure 1). Present water quality conditions at these sites are compared to baseline water quality conditions collected over the period of 2008 to 2012. Figure 1 - Upper Cache la Poudre Collaborative Monitoring Program sampling locations Water Quality Update | Spring 2020 Monitoring and Protecting Our Water Sources DocuSign Envelope ID: A197C63C-385D-42DB-97DD-4FEEEB336D55 TEMPERATURE Air temperature measured at the Joe Wright SNOTEL over the 2020 spring season was 3.1°F warmer than the long- term average and ranked as the fourth warmest spring on record. The monthly mean air temperatures for March, April and May were all above the long-term average. The months of March and May were particularly warm and ranked as the fifth and second warmest on record (Table 1). Water Quality Update | Spring 2020 fcgov.com/water-quality Table 1 – Monthly mean air temperatures measured at Joe Wright SNOTEL over the spring months of 2020 compared to the long-term average (1990 – 2019). PRECIPITATION Precipitation measured at the Joe Wright SNOTEL over the 2020 spring season was 80% of the long-term average and ranked as the ninth driest spring on record. All spring months measured below average. The largest deficit in the monthly total precipitation was observed in the month of May, which measured 72% of average (Table 2). Table 2 – Monthly accumulated precipitation totals measured at the Joe Wright SNOTEL over the 2020 spring season compared to the long-term average (1981–2010). Note: W = wettest and D = driest Period of Record Temperature 2020 (ºF) Average (ºF) Departure (ºF) 2020 Rank March 29.0 25.0 4.0 5th (H) April 32.0 30.5 1.5 12th (H) May 42.0 38.3 3.7 2nd (H) Spring 34.3 31.3 3.1 4th (H) Period of Record Total Precipitation 2020 (inches) Average (inches) % average 2020 Rank March 3.8 4.7 80% 12th (D) April 4.5 5.2 87% 16th (D) May 3.2 4.5 72% 14th (D) Spring 11.5 14.4 80% 9th (D) DocuSign Envelope ID: A197C63C-385D-42DB-97DD-4FEEEB336D55 Water Quality Update | Spring 2020 fcgov.com/water-quality SNOWPACK Snow water equivalent (SWE), the amount of water held in the snowpack, was above normal at snow telemetry stations (SNOTEL) throughout the Upper CLP watershed. The Joe Wright SNOTEL near Cameron Pass was below the long-term (1981–2010 median (normal)) for most of the snow accumulation season. A series of potent winter storms from late-January through early-February delivered 4-6 feet of snow to the mountains in the Upper CLP watershed. SWE measured above normal following this storm cycle and remained above normal through the remainder of the snow accumulation season. The maximum amount of water contained in the snowpack, referred to as peak SWE, was observed on April 28 at the Joe Wright SNOTEL and measured at 25.3 inches – 108% of normal (Figure 2). Figure 2 – Peak snow water equivalent measured at SNOTEL sites throughout the Upper Cache la Poudre River watershed in 2020. DocuSign Envelope ID: A197C63C-385D-42DB-97DD-4FEEEB336D55 Water Quality Update | Spring 2020 fcgov.com/water-quality Figure 3 – Streamflow conditions on the Poudre River over the 2020 spring season (left) and monthly total water volume measured over the spring season (right). STREAMFLOW CONDITIONS Streamflow at the Cache la Poudre River near the Canyon Mouth (CLAFTCCO) stream gage measured 62,785 acre- feet over the spring season, which was slightly below the long-term average (93%). Streamflow was near average in March (103%) and below average in April (80%) and May (93%) (Figure 3). There was a slight delay in the start of snowmelt runoff in 2020, but streamflow rapidly began to rise in early May. Cooler weather in late-May briefly slowed snowmelt runoff but hot weather followed, and streamflow quickly increased above the long-term average. In 2020, peak streamflow was measured on June 1 at 3,020 cubic feet per second (cfs). Peak streamflow occurred 10 days earlier than average and measured approximately 150% of the long-term average peak streamflow. DocuSign Envelope ID: A197C63C-385D-42DB-97DD-4FEEEB336D55 The Upper Cache la Poudre Collaborative Water Quality Monitoring Program uses several key water quality indicators, including pH, conductivity, temperature and turbidity, which act as surrogates for other parameters. (Table 2). These indicators provide a snapshot of water quality conditions and are useful for identifying trends or changes in water quality. Significant changes in water quality indicators may provide an early warning of potential water pollution. Water Quality Update | Spring 2020 fcgov.com/water-quality WATER QUALITY INDICATORS Table 2 – Water quality indicators measured as part of the Upper Cache la Poudre Collaborative Water Quality Monitoring Program. Water Quality Indicator Explanation Temperature Water temperature influences other water quality parameters and is a major driver of biological activity and algal growth in rivers, including certain phytoplankton species that produce the taste and odor compounds, geosmin and 2-methlyisoborneol. pH pH is an important water quality parameter to monitor, because it influences the solubility and biological availability of chemical constituents, including nutrients and heavy metals. pH near 7 is considered neutral, with more acidic conditions occurring below 7 and more basic, or alkaline, conditions occurring above 7. Specific Conductivity Conductivity is an index of dissolved ionic solids in water. Conductivity is used as a general measure of water quality. Significant increases in conductivity can be used as an indicator of increased pollution. Turbidity Turbidity is monitored to track changes in water clarity. Clarity is influenced by the presence of algae and/or suspended solids introduced to surface waters through various land use activities, including runoff and erosion, urban stormwater runoff and drainage from agricultural lands. For water treatment, turbidity is an important indicator of the amount of suspended material that is available to harbor pollutants, such as heavy metals, bacteria, pathogens, nutrients and organic matter. DocuSign Envelope ID: A197C63C-385D-42DB-97DD-4FEEEB336D55 Water Quality Update | Spring 2020 fcgov.com/water-quality Figure 4 – Water quality indicator data collected at key monitoring sites over the 2020 spring monitoring season (April and May) compared to baseline spring water quality conditions. Spring water quality monitoring captures water quality conditions from the start of snowmelt runoff to peak streamflow. Water quality conditions vary with changes in elevation and contributing watershed area. Water quality indicators on the Mainstem CLP River near the City of Fort Collins’ (PNF) and City of Greeley’s (PBD) water supply intakes measured within the range of baseline conditions, indicating normal water quality conditions on the Poudre River during the spring 2020 snowmelt runoff season (Figure 4). Water temperature was slightly higher than baseline. pH and specific conductivity were near baseline on the Mainstem CLP River near the City of Fort Collins’ water supply intake (PNF) and higher than the baseline on the Mainstem CLP River near the City of Greeley’s intake (PBD). Turbidity was higher than baseline at both monitoring locations. WATER QUALITY INDICATORS CONTINUED DocuSign Envelope ID: A197C63C-385D-42DB-97DD-4FEEEB336D55 Water Quality Update | Spring 2020 fcgov.com/water-quality TASTE AND ODOR COMPOUNDS Geosmin and 2-Methylisoborneol (MIB) are naturally occurring organic compounds that introduce an earthy odor to water that can be detected by the most sensitive individuals at concentrations as low as 4 nanograms per liter (ng/L) or 4 parts per trillion (ppt). These compounds do not pose a public health risk but are of concern because their detectable presence can negatively affect customer confidence in the quality of drinking water. Geosmin and 2-MIB are monitored at PBR and PNF during routine UCLP monitoring events. Geosmin was detected at the City of Fort Collins’ water supply intake (PNF) on May 26, but was only slightly above the water quality laboratory’s reporting limit of 2 ng/L. 2-MIB was not detected above the water quality laboratory’s reporting limit (5 ng/L). Casey Barby, Watershed Technician, collects water quality indicator data on the North Fork Cache la Poudre River in early spring using a multi-parameter water quality sonde. DocuSign Envelope ID: A197C63C-385D-42DB-97DD-4FEEEB336D55 Water Quality Update | Spring 2020 fcgov.com/water-quality 2019 UPPER CACHE LA POUDRE WATERSHED WATER QUALITY REPORT The Upper Cache la Poudre Watershed Collaborative Monitoring Program recently released its 2019 Annual Report. It summarizes climate and hydrology in the Upper CLP watershed in 2019 and water quality data collected as part of the Upper CLP Collaborative Water Quality Monitoring Program. Water quality reports can be found online at fcgov.com/source-water-monitoring/. DocuSign Envelope ID: A197C63C-385D-42DB-97DD-4FEEEB336D55