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HomeMy WebLinkAboutMemo - Mail Packet - 7/25/2017 - Memorandum From Jared Heath Re: 2017 Spring Water Quality Update - Upper Cache La Poudre WatershedUtilities electric · stormwater · wastewater · water 700 Wood Street PO Box 580 Fort Collins, CO 80522 970.221.6700 970.221.6619 – fax 970.224.6003 – TDD utilities@fcgov.com fcgov.com/utilities M E M O R A N D U M DATE: July 14, 2017 TO: Mayor Troxell and Councilmembers FROM: Jared Heath, Watershed Specialist THRU: Darin Atteberry, City Manager Kevin R. Gertig, Utilities Executive Director RE: 2017 Spring Water Quality Update – Upper Cache la Poudre Watershed Bottom Line: In the shared interest of monitoring the Upper Cache la Poudre (Upper 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 overarching 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 brief summary of snowpack and streamflow, and water quality conditions monitored in the Upper CLP watershed during the spring months of April, May, and June in 2017. 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 2017 Highlights: The Upper CLP watershed continues to be a reliable, high quality drinking water source. Water quality during snowmelt runoff in the spring is typically more variable than other times of the year. Normal water quality conditions were observed throughout the Upper CLP watershed during the 2017 snowmelt runoff season. CC: Carol Webb, Water Resources and Treatment Operations Manager, Utilities Jill Oropeza, Water Quality Services Manager, Utilities DocuSign Envelope ID: D184330C-8B03-48EF-A3F9-453420876FCD Water Quality Update | Spring 2017 fcgov.com/water-quality Monitoring and Protecting Our Water Sources SOURCE WATER MONITORING JWC - Joe Wright Creek above the confl uence with the Poudre River PJW - Poudre River above the confl uence with Joe Wright Creek PBR - Poudre River below the Town of Rustic PSF - Poudre River below the confl uence with the Little South Fork PNF - Poudre River above the confl uence with the North Fork at the City of Fort Collins’ Intake PBD - Poudre River below the confl uence 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 2017 Water Quality Update provides a seasonal summary of watershed conditions in the Upper CLP Watershed by highlighting snowpack and streamfl ow conditions, as well as water quality information collected over the months of April, May and June. Water quality during snowmelt runoff is highly variable and to better capture this seasonal variability, monitoring is conducted two times per month from April through June. Results are reported for six key monitoring sites located throughout the Upper Cache la Poudre watershed, which capture water quality conditions above and below major tributaries and near water supply intake structures (Figure 1). More information is available at fcgov.com/source-water-monitoring. Figure 1 - Upper Cache la Poudre Collaborative Monitoring Program sampling locations DocuSign Envelope ID: D184330C-8B03-48EF-A3F9-453420876FCD Snow water equivalent (SWE), the amount of water held in the snowpack, measured at Joe Wright snow telemetry station near Cameron Pass was below the long-term median during the start of the snow accumulation season. In normal years the snowpack begins to develop in October and steadily accumulate through April. Dry and warm conditions that began in the summer of 2016 persisted through the months of October and early November with the snow accumulation season beginning nearly six weeks later than normal. Steady storms beginning in mid-November through December brought the snowpack back to near normal conditions. A strong storm during the fi rst week of January increased the amount of water in the snowpack from 7.6 inches to 12.8 inches leaving the snowpack well above normal (Figure 2a). The water content in the snowpack remained above normal through February, but the rate of accumulation during these months was slower than normal resulting in near normal conditions by early March. Variably dry and wet conditions beginning in March resulted in periods of snowmelt and snow accumulation cycles before the water content peaked in May. The maximum amount of water contained in the snowpack, referred to as peak SWE, at Joe Wright SNOTEL was measured on May 4 at 19.5 inches – 83 percent of the historical median (Figure 2a). Based on the 30 year period of record, peak SWE at Joe Wright SNOTEL normally occurs on April 29. Peak SWE varied throughout the Upper CLP watershed (Figure 3). The North Fork and Mainstem Poudre were near the historic median, while the Little South Fork watershed measured below the historic median. Peak SWE for the Upper CLP basin was measured at 103 percent of the median for the 2017 water year. Water Quality Update | Spring 2017 fcgov.com/water-quality SNOWPACK AND STREAMFLOW CONDITIONS Figure 2 – Snowpack (a) and streamfl ow (b) conditions in the Poudre River watershed over the 2017 water year. Sep Aug Jul Jun May Apr Mar Feb Jan Dec Nov Oct 20 15 10 5 0 WATERYEAR SWE (inches) Median (1981-2010) WY2017 Explanation a) Cache la Poudre SnowWater Equivalent at Joe Wright Sep Aug Jul Jun May Apr Mar Feb Jan Dec Nov Oct 3000 2000 1000 Water Quality Update | Spring 2017 fcgov.com/water-quality SNOWPACK AND STREAMFLOW CONDITIONS Figure 3 - Percent of median peak snow water equivalent at snow monitoring sites throughout the Upper Cache la Poudre River watershed. Snowmelt runoff began in early May, which was slightly later than normal. Streamfl ow, as measured at the Canyon Mouth, followed closely to the historic average. A late winter storm in May delivered signifi cant snow to the mid and lower elevations of the North Fork and Main- stem watersheds. This storm was followed by warmer weather and a rain-on-snow event which accelerated snow- melt causing a rapid rise and initial peak in streamfl ow. Streamfl ow increased from about 1,000 cubic feet per sec- ond (cfs) to 2,500 cfs in seven days. Streamfl ow receded following this event, but quickly increased from snowmelt occurring higher in the watershed. Peak streamfl ow (daily average) was observed on June 11 at 3,140 cfs – 157 percent of the average peak stream- fl ow. The snowpack at Joe Wright SNOTEL was completely melted by June 16 and by the June 20 monitoring event, streamfl ow had receded to normal streamfl ow levels (Figure 2b). DocuSign Envelope ID: D184330C-8B03-48EF-A3F9-453420876FCD The Upper Cache la Poudre Collaborative Water Quality Monitoring Program tests for several key water quality indicators, including pH, conductivity, temperature and turbidity (Table 1). These key measurements provide a snapshot of water quality conditions, which are useful to identify trends or changes in water quality. Signifi cant changes in water quality may provide an early warning of potential water pollution. Water Quality Update | Spring 2017 fcgov.com/water-quality WATER QUALITY INDICATORS Temperature Water temperature infl uences 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 compound, geosmin. Water Quality Indicator Explanation pH pH is an important water quality parameter to monitor, as it infl uences 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. Specifi c Conductivity Conductivity is an index of dissolved ionic solids in water. Hardness is an index of the total calcium (Ca) and magnesium (Mg) in water. Turbidity Turbidity is monitored to track changes in water clarity. Clarity is infl uenced 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. Spring water quality monitoring captures water quality conditions throughout snowmelt runoff and peak streamfl ow. Water quality conditions vary with changes in elevation and contributing watershed area. All water quality indicators at key sites reported near the long-term median, indicating normal water quality conditions on the Poudre River during the 2017 snowmelt runoff season (Figure 4). The following lists the range of values measured throughout the Mainstem watershed during spring water quality monitoring in 2017: • Water temperature = 0.1º C – 13.6º C • pH = 6.85 – 8.20 • Specifi c conductivity = 21.4 μS/cm – 109.4 μS/cm • Turbidity =1.4 NTU – 14.0 NTU Jorin Botte collects a grab sample on Joe Wright Creek below Chambers Lake. Table 1 - Water quality indicators measured as part of the Upper Cache la Poudre Collaborative Water Quality Monitoring Program. DocuSign Envelope ID: D184330C-8B03-48EF-A3F9-453420876FCD Water Quality Update | Spring 2017 fcgov.com/water-quality fcgov.com/water-quality WATER QUALITY INDICATORS CONTINUED Maximum Median Minimum Graphic Explanation Data range based on long-term data record 2008-2016. Figure 4 – Water quality indicator data collected at key monitoring sites during Spring (April, May, June) 2017. All water quality indicators at key sites reported near the long-term median, indicating normal water quality conditions. JWC PJW PBR PSF PNF PBD 20 15 10 5 0 TEMP (deg C) JWC PJW PBR PSF PNF PBD 9 8 7 6 pH JWC PJW PBR PSF PNF PBD 200 150 100 50 0 CONDUCTIVITY (uS/cm) JWCPJWPBRPSF PNF PBD 30 20 10 0 TURBIDITY (NTU) Spring Median (2017) Joe Wright Creek Canyon Mouth Joe Wright Creek Canyon Mouth DocuSign Envelope ID: D184330C-8B03-48EF-A3F9-453420876FCD Water Quality Update | Spring 2017 fcgov.com/water-quality fcgov.com/water-quality MICROORGANISMS Figure 5 – E. coli (a) and (b) T. coli counts on the Poudre River during the 2017 Spring water quality monitoring. Through the UCLP Collaborative Monitoring Program, the Poudre River is routinely tested for the presence of bacterial contamination by measuring the total amount of coliforms, an indicator organism for the presence of pathogenic bacteria. In addition, Escherichia coli (E. coli) is measured and used as an indicator of human or animal fecal waste pollution since the source of origin is more specifi c than total coliforms. During the spring, snowmelt and rain serve as delivery mechanisms for E. coli and total coliforms from the surrounding watershed to the Poudre River. Over the Spring 2017 monitoring season, E. coli and total coliforms were within the range of values seen in previous years, but slightly higher than the long-term median (Figure 5a, 5b). E. coli counts ranged from no detection to 579 cells per milliliter and total coliform ranged from 57 to 1,633 cells per milliliter. The highest E. coli count was observed at PNF on April 10, which was the maximum E. coli count observed over the eight year monitoring record. Cell counts were measured nearly two orders of magnitude lower (5.2 cells per milliliter) on the following event on April 24 and remained notably lower in subsequent spring monitoring events in May and June. E. coli and total coliforms remained within the range of values seen in previous years, but were slightly higher than the long-term median. PBR PSF PNF PBD 400 300 200 100 0 CELLS/mL PBR PSF PNF PBD 2000 1500 1000 500 0 CELLS/mL a) E. coli b) Total coliforms DocuSign Envelope ID: D184330C-8B03-48EF-A3F9-453420876FCD The Upper Cache la Poudre Watershed Collaborative Monitoring Program recently released its 2016 Annual Report, which summarizes the hydrologic and water quality data collected in 2016 and provides a comparison of water quality from the years 2013-2016. The report also summarizes signifi cant events, issues of concern, results from special studies, and data quality control. Water quality reports can be found online at fcgov.com/source-water-monitoring. Water Quality Update | Spring 2017 fcgov.com/water-quality 2016 UPPER CACHE LA POUDRE WATERSHED ANNUAL REPORT DocuSign Envelope ID: D184330C-8B03-48EF-A3F9-453420876FCD 0 WATERYEAR STREAMFLOW(CFS) Historic Av erage (135 Year Record) WY2017 Spring WQ sampling Explanation b) Cache la Poudre Streamflowat Canyon Mouth DocuSign Envelope ID: D184330C-8B03-48EF-A3F9-453420876FCD