ГлавнаяMy WebLinkО нас02-2016 Cayuga Lake Modeling Project UpdateCayuga Lake Modeling Project Update February 2016 Liz Moran, EcoLogic Presentation Outline • Description of the Cayuga Lake Modeling Project – Relation to Lake Source Cooling permit renewal – Project team • Findings to Date: February 2016 – Sources of phosphorus and bioavailability – Lake hydrodynamics • Model Development Status • Implications and Next Steps February 2016 2 Presentation Outline • Description of the Cayuga Lake Modeling Project – Relation to Lake Source Cooling permit renewal – Project team • Findings to Date – Sources of phosphorus and bioavailability – Lake hydrodynamics • Model Development Status • Implications and Next Steps February 2016 3 Photos, illustrations, graphics here.Cayuga Lake Modeling Project (CLMP) • Scientific investigation of sources of phosphorus to Cayuga Lake and the consequences for phytoplankton growth • Does not model aquatic plants (macrophytes) • Included as a permit requirement for operation of Cornell’s Lake Source Cooling (LSC) facility February 2016 4 Why investigate the sources and impacts of phosphorus in Cayuga Lake? • Phosphorus is the limiting nutrient for phytoplankton growth • In 2002, DEC listed southern Cayuga Lake as impaired by excessive phosphorus and silt/sediment – Impaired relative to a designated “best use” – In 2008, southern lake listed for pathogens, delisted in 2014 based on City and CSI data • Once southern Cayuga Lake was listed as impaired, DEC was required to act – Identify and quantify the source(s) of impairment – Identify strategy for improvement- TMDL or other February 2016 5 4- Class A 3- Class AA (T) 1- Class B NYSDEC classifies Cayuga Lake in four distinct segments, depending on “best use”, and habitat suitability for salmonids, designated by (T) 2- Class A(T) 6 Best Use: AA A B Water supply- minimal treatment Water supply-coagulation & filtration Water contact recreation Fishing Fish, shellfish & wildlife propagation and survival February 2016 CLMP focuses on phosphorus (P) and algae • Southern shelf listed as impaired due to occasional exceedances of Total P guidance value – 20 µg/L summer average • Guidance value selected to protect recreational uses in Class AA, A, and B lakes from excessive algae (phytoplankton) • Sediment not a direct focus of CLMP, only as it contributes to biologically-available P and affects water clarity February 2016 7 Why is the CLMP included as a permit condition for operation of the LSC facility? • LSC draws cold water from deep in the lake—segment 3, circulates it through a shoreline heat exchange facility, and returns water (slightly warmed) to segment 4 • No phosphorus is added • Assuming that deep & shallow lake waters do not naturally mix during summer, DEC considered LSC a point source of phosphorus to segment 4 (the shelf) February 2016 8 The Lake Source Cooling Process February 2016 9 Environmental Benefits of the LSC Facility • Renewable resource • Energy efficiency – 86% reduction in energy used for cooling of campus and Ithaca High School – Overall reduction of campus energy use by 10% – Decreased reliance on fossil fuels & reduced adverse impacts, including greenhouse gases • Cornerstone of University’s commitment to sustainability: multiple awards February 2016 10 Cornell Perspective on CLMP Requirement • Willing to invest in research and modeling to support a rational management approach – Integrate science into policy decisions: CU mission – Draw on local knowledge – Collaborate with DEC to apply an emerging approach that considers impacts on water, air, and lands • Committed to continued operation of the LSC facility February 2016 11 Elements of the CLMP • Phase 1: Monitoring (April 2013 – Oct 2013) – Project plan reviewed and approved – Testing streams, lake, point sources – Lake biological community- mussels and plankton – Bioavailability of phosphorus fractions • Phase 2: Modeling (Jan 2014 – Dec 2016) – Watershed model: effects of land use, land cover, and hydrology on phosphorus flux – Lake model: water circulation (hydrodynamics) and water quality, focus on phosphorus and algae February 2016 12 Project Partners • DEC and EPA: Oversight & Approvals – DEC: Technical Advisory Committee – EPA: Model Evaluation Group • Cornell: Project Execution – Provide funding – Develop and manage technical team • Community stakeholders: Review & Advisory – Led by County Water Resources Council’s Lake Monitoring Partnership • Data sharing partners – Community Science Institute, City of Ithaca, Watershed Network, Researchers February 2016 13 CLMP Technical Team • Upstate Freshwater Institute – Lake and stream monitoring, lake water quality model • Dr. Todd Cowen- Cornell Hydraulics Lab – Hydrodynamic model • Dr. Todd Walter- NY Water Resources Institute – Watershed model- phosphorus & sediment loss from landscape to lake • Drs. Nelson Hairston, Lars Rudstam & Jim Watkins – Phytoplankton and zooplankton – Zebra and quagga mussels • EcoLogic – Communication among DEC, Cornell project team, & community February 2016 14 Presentation Outline • Description of the Cayuga Lake Modeling Project – Relation to Lake Source Cooling permit renewal – Project team • Findings to Date – Sources of phosphorus and bioavailability – Lake hydrodynamics • Model Development Status • Implications and Next Steps February 2016 15 Findings to Date (February 2016) • Phosphorus fractions (dissolved, particulate, etc.) differ in bioavailability, i.e., the ability to support algal growth • Detailed monitoring and analysis in 2013 reveal that nearly all bioavailable phosphorus to Cayuga Lake came from watershed nonpoint sources (97%), not point sources (3%) • Elevated total phosphorus concentrations are associated with sediment particles (mud) that enter the lake during runoff events, and the mud has low bioavailability • Lake circulation is complex and dynamic, with significant mixing between the southern shelf and the main lake February 2016 16 April – October 2013 Bioavailable P Inputs, Shelf and Lake-wide Bioavailable P Load to Bioavailable P Load to Shelf: 3.4 mt Cayuga Lake: 13.8 mt 2 Treatment Plants (IA,CH) 7% LSC recirculation 6% Tributaries LSC (recirculation) Tributaries 87% 6 Treatment Plants 3% Tributaries 97% Tributaries Treatment Plants Treatment Plants (IA,CH) February 2016 17 TP (µg/L) 0 10 20 30 40 Jun Jul Aug Sep Q (m3 /s) 0 20 40 60 80 100 Runoff delivers sediment “mud” to the shelf, but phosphorus (PP m/u) in mud is very low in bioavailability hydrology cases of interest dry weather runoff events s ml s ml s ml PPm/u wet summer case 2013 dry weather runoff events summer average Green-total dissolved P+ particulate organic P s – shelf Red-particulate inorganic P (mud) ml- main lake All fractions contribute to Total P (TP) February 2016 18 Sediment Plume from Taughannock Creek Photo: Bill Hecht February 2016 19 Complex Lake Circulation Patterns Photo: Bill Hecht February 2016 20 Wind-driven circulation brings deep water onto the shelf February 2016 21 Natural mixing processes prevent development of higher phytoplankton biomass on the shelf barrier scenario response would be different if the shelf was a separate lake in series with Cayuga Lake much slower flushing rate; could increase local phytoplankton local loads shelf mixing flushing rate of shelf from mixing is rapid relative to phytoplankton growth rates (Effler et al. 2010, Gelda et al. 2015a) local loads Recent upgrades to the Cayuga Heights and Ithaca WWTPs reduced bioavailable P load by ~80% with no response in chlorophyll-a. This is attributed to the rapid flushing of the shelf from natural mixing processes February 2016 22 Chlorophyll-a Concentrations Shelf & Main Lake 0.0 1.0 2.0 3.0 4.0 5.0 6.0 7.0 8.0 9.0 1998 1999 2000 2001 2002 2003 2004 2005 2006 2007 2008 2009 2010 2011 2012 2013 Chlorophyll‐a, ug/L Shelf Main Lake February 2016 23 Presentation Outline • Description of the Cayuga Lake Modeling Project – Relation to Lake Source Cooling permit renewal – Project team • Findings to Date – Sources of phosphorus and bioavailability – Lake hydrodynamics • Model Development Status • Implications and Next Steps February 2016 24 Status of Watershed Model • Model of phosphorus transport from the watershed to the lake – Multiple fractions of P, to interface with lake model – Adapted SWAT-VSA to track storm runoff – Informed by detailed assessment of agricultural practices in Fall Creek subwatershed • Working closely with County Soil & Water Conservation Districts and others to define realistic management scenarios February 2016 25 Fall Creek Phosphorus Export Detailed analysis: • Soils • Slopes • Wetness factor • Land cover • Agricultural practices including manure disposal February 2016 26 Building the Overall Phosphorus: Water Quality Model To date, UFI and their collaborators have submitted 11 scientific papers to peer-reviewed journals based on their Cayuga Lake investigations (9 accepted, 2 in review) February 2016 27 Presentation Outline • Description of the Cayuga Lake Modeling Project – Relation to Lake Source Cooling permit renewal – Project team • Findings to Date – Sources of phosphorus and bioavailability – Lake hydrodynamics • Model Development Status • Implications and Next Steps February 2016 28 Implications • Reconsider whether southern Cayuga Lake is impaired by phosphorus: – Total P is a flawed indicator of algal growth potential, dominated by muds with low bioavailability – Extensive water exchange between shelf and main lake – Massive (80%) reduction in point source bioavailable P has not reduced chlorophyll-a • What other management methods are appropriate, given these findings? February 2016 29 Next Steps • Continue to work with NYSDEC to advance the scientific basis for lake management – Sharing data and publications with DEC and EPA • Advocate for a robust watershed management approach to protect Cayuga Lake that reflects the detailed scientific investigations February 2016 30 All Reports, Presentations, Technical Papers and Data are on the Cayuga Lake Modeling Project Webpage www.cayugalakemodelingproject.cornell.edu February 2016 31 Thank You Questions and Discussion February 2016 32