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Cayuga Lake Modeling Project
Update
March 2016
Liz Moran, EcoLogic
Photo: Bill Hecht
• Description of the Cayuga Lake Modeling Project
– Relation to Lake Source Cooling permit renewal
– Project team
• Findings to Date: Cayuga Lake
– Sources of phosphorus and bioavailability
– Water circulation (hydrodynamics)
• Watershed Model Status
• Major Findings and Next Steps
Presentation Outline
March 2016 2
• Description of the Cayuga Lake Modeling Project
– Relation to Lake Source Cooling permit renewal
– Project team
• Findings to Date: Cayuga Lake – Sources of phosphorus and bioavailability
– Water circulation (hydrodynamics)
• Watershed Model Status
• Major Findings and Next Steps
Presentation Outline
March 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
March 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 impairedby 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
March 2016 5
4- Class A
3- Class AA (T)
1- Class BNYSDEC 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
March 2016
March 2016 7
• Southern shelf listed as impaired due to occasional
exceedances of DEC’s 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
CLMP focuses on Phosphorus (P) and Algae
• 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)
Why is the CLMP included as a permit condition for
operation of the LSC facility?
March 2016 8
The Lake Source Cooling Process
March 2016 9
Environmental Benefits of the LSC Facility
• Renewable resource
– Decreased reliance on fossil fuels & reduced adverse impacts,
including greenhouse gases
• Energy efficiency
– 86% reduction in energy used for cooling of campus and
Ithaca High School
• Reduced demand on electrical grid
– 25 million kW hrs/year
– Reduced load at peak demand periods
March 2016 10
• CLMP represents a significant investment in research
and modeling
• Integrate science into policy decisions for managing
Cayuga Lake and other lakes
• Holistic evaluation of all the sources of P and how they
affect the lake
• Apply the emerging ecosystem-based management
approach that considers impacts on water, air, and lands
Opportunities to Advance Science and Policy
March 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
– Measure bioavailability of phosphorus fractions
• Phase 2: Modeling (Jan 2014 – Dec 2016)– Lake model: water circulation (hydrodynamics) and water
quality, focus on phosphorus and algae
– Watershed model: effects of land use, land cover, and hydrology on phosphorus flux
March 2016 12
March 2016 13
Project PartnersNYSDEC
Cornell University
Utilities & Energy Management
Upstate Freshwater Institute
(Monitoring and Lake Model)
Cornell BEE
Soil & Water Lab
(Watershed Model)
Faculty Advisors
Technical Advisory
Committee
USEPA
Model Evaluation
Group
Oversight & Approvals
Project Management
and Funding
Model Developers
• Description of the Cayuga Lake Modeling Project
– Relation to Lake Source Cooling permit renewal
– Project team
• Findings to Date: Cayuga Lake – Sources of phosphorus and bioavailability
– Water circulation (hydrodynamics)
• Watershed Model Status
• Major Findings and Next Steps
Presentation Outline
March 2016 14
• 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 entering 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
Findings to Date (March 2016)
March 2016 15
April – October 2013
Bioavailable P Inputs, Shelf and Lake-wide
Tributaries
97%
6 Treatment
Plants
3%
Bioavailable P Load to
Cayuga Lake: 13.8 mt
Tributaries Treatment Plants
Tributaries
87%
LSC recirculation
6%
2 Treatment
Plants
(IA,CH)
7%
Bioavailable P Load to
Shelf: 3.4 mt
Tributaries
LSC (recirculation)
Treatment Plants
(IA,CH)
March 2016 16
TP
(µ
g/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 (base flow)runoff events
dry weather runoff events summer average
s – shelf
ml- main lake
s ml s ml sml
PPm/u wet
summer
case
March 2016 17
Green- total dissolved P+ particulate organic P
Red- particulate inorganic P (mud)
All fractions contribute to Total P (TP)
2013
Sediment Plume from Taughannock Creek
Photo: Bill Hecht
March 2016 18
Complex Lake Circulation Patterns
Photo: Bill Hecht
March 2016 19
March 2016 20
Wind-driven circulation brings deep water onto the
shelf
Natural mixing processes prevent development of
higher phytoplankton biomass on the shelf
shelf
mixing
local loads
“Flushing rate of the shelf from mixing is rapid relative to phytoplankton growth rates”
(Effler et al. 2010, Gelda et al. 2015a)
Recent upgrades to the Cayuga Heights and Ithaca treatment plants reduced bioavailable P load by ~80% from those point sources with no response in algae.
This is attributed to the rapid flushing of the shelf from natural mixing processes.
March 2016 21
March 2016 22
Chlorophyll-a Concentrations (Measure of Algae)
are Comparable at Shelf & Main Lake Stations
0
2
4
6
8
10
12
14
16
Ch
loro
ph
yll
-a, u
g/L
Shelf Main Lake
• Description of the Cayuga Lake Modeling Project
– Relation to Lake Source Cooling permit renewal
– Project team
• Findings to Date: Cayuga Lake – Sources of phosphorus and bioavailability
– Water circulation (hydrodynamics)
• Watershed Model Status
• Major Findings and Next Steps
Presentation Outline
March 2016 23
March 2016 24
• Estimate phosphorus loads
from the watershed
– Inform lake model inputs
• Provide a tool to test
management (“what-if”)
scenarios
Objectives of the Watershed Model
Model Choice and Rationale
Soil Water Assessment Tool (SWAT)
Developed by USDA-ARS, Texas A&M
Widely used in TMDL-type projects
Simulates dissolved & particulate P
Soil & Water team experienced
with SWAT model
Adaptable to local conditions
Flexible management input
Goog
le Im
ages
4
March 2016 25
Dave
Bouldin
CSI
26
Photos, illustrations, graphics here.
March 2016 27
Land Use/Land Cover Affect
Phosphorus Export
• Streams draining
agricultural areas have
higher phosphorus
concentrations
• Forested landscapes
have much lower
phosphorus loss
% Forest
% Agriculture
Tota
l P
(m
g/L
)
100%
100%0%
0%
0.00
0.30
Lyon, Walter, et al. 2006. JAWRA. 42(3): 793-804
Watershed Model Data Needs
• Fraction of agricultural lands managed by
larger farms vs. smaller farms
• Rate of application of manure
• Frequency and timing of manure application
per managed unit (field)
31
March 2016 28
• Soil and Water Conservation Districts
• Ag & Markets / Pro-Dairy
• NYS Soil and Water Conservation Committee
Manure Management: Data Sources
March 2016 29
March 2016 30
• CAFO (350 cows)- Manure storage – Apply to row crops (e.g., corn) in May and October
– Apply to hay lands in May and October
– Some hay lands may receive manure in other months
• AFO (Fewer than 350 cows)– Apply to row crops in May and October
– Apply to hay lands year round; one annual spread per field
• Overall, 30% of hay lands receive manure in any one year
Manure Management: Detailed Findings
1990
Fal
l C
reek
Dis
char
ge,
m3/s
ec
March 2016 31
1978
Some Total Phosphorus ResultsT
ota
l P
ho
sphoru
s, k
g/d
ay
March 2016 32
Fall Creek Phosphorus Export
Detailed analysis:
• Soils
• Slopes
• Wetness factor
• Land cover
• Agricultural practices
including manure
disposal
March 2016 33
Scenarios
• Current conditions
• Hindcast: What were sediment and phosphorus loads pre-settlement (1700s)?
• Management:
– Turn off individual sources
– Implement agricultural Best Management Practices
• Change the timing of manure applications ~ avoid forecasted rain
• Change the placement of manure ~ buffers around concentrated flow paths
• Other recommended practices ~ cover crops, swales
• Forecast: Potential changes in a future climate
March 2016 34
Looking Ahead
• 2016
– Lake eutrophication model
– Watershed model
– Linkage between lake and watershed models
– Models delivered to NYSDEC for their use
• 2017
– NYSDEC will develop TMDL for southern Cayuga, or identify other effective water quality strategies
March 2016 35
• Description of the Cayuga Lake Modeling Project
– Relation to Lake Source Cooling permit renewal
– Project team
• Findings to Date: Cayuga Lake – Sources of phosphorus and bioavailability
– Water circulation (hydrodynamics)
• Watershed Model Status
• Major Findings and Next Steps
Presentation Outline
March 2016 36
• The shelf is not a separate manageable water body
• Tributary streams (watershed) are the overwhelming
source of bioavailable phosphorus
• Extensive monitoring data indicate that Cayuga Lake
water quality is consistent with a mesotrophic
(healthy) condition with no trend to degradation
• Lake clarity is reduced after storms by sediment, not
algae
Major Findings to Date
March 2016 37
• Watershed model will provide quantitative tool for assessing phosphorus sources and potential reductions
• Watershed model to inform lake model- what is the impact of potential reductions?
• Opportunity to apply this detailed knowledge to the Watershed Management Plan update now underway
– 20+ scientific papers from UFI and Soil & Water Lab
– Potential to apply CLMP knowledge far beyond Cayuga watershed
Next Steps
March 2016 38
www.cayugalakemodelingproject.cornell.edu
All Reports, Presentations, Technical Papers and Data
are on the Cayuga Lake Modeling Project Webpage
March 2016 39
Thank You
Questions and Discussion
March 2016 40