an advanced atmosphere/ocean assessment program: reducing the risks associated with offshore wind...
TRANSCRIPT
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State of New JerseyNew Jersey Board of Public Utilities (NJBPU)
An Advanced Atmosphere/Ocean Assessment Program:
Reducing the Risks Associated with Offshore WindEnergyDevelopment
As Defined by The NJ Energy Master Plan andThe NJ Offshore Wind Energy Economic Development Act
Principal
Investigators: Scott Glenn, Sc.D. and Rich Dunk, Ph.D., CCMTeam Members:Josh Kohut, Louis Bowers, Greg Seroka, John Kerfoot, Lisa
Ojanen, Ethan Handel
Hi-Res Weather
ModelSpatial
Validation DataWind Power
Statistics
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Ecological baselinestudies of offshorewind power alreadyperformed
Avian species
Fisheries Marine Mammals Sea turtles
This project willperform physical
baseline study
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NJDEP Ecological Sensitivity andAWS Truewind Resource Map
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Risks1. Wind farm design:
What is the optimal spacing of wind turbines?
1. Installation:
When is the best time to install planned and futurewind turbines?
1. Operation:
When do you schedule maintenance? How do youforecast power for the day-ahead market?
1. Planning:
Where do we site future wind turbines?
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Risk reductionWe will develop an
improved weather modeland spatial datasets for:
1. Design and installation ofexisting wind farms
2. Comparison with ecological
studies for siting of future windfarms
3. Future operations andmaintenance of wind farms
4. More accurate day-aheadforecasts for the energy market
90 m Annual Wind Speed (m/s) andDirection from RU-WRF
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Why do we need a betteratmospheric model?Seasonal Sea Surface Temperature
NJ Sea Breeze
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Large-Scale and Small-ScaleOffshore WindOur experience with both atmospheric and oceanographic
monitoring and modeling will provide the best estimates of offshorewind along the coast of New Jersey.
Infrared SatelliteWeather Radar
RU-WRF Model 2kmSimulation
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Operational Mesoscale Modelingwith RU-WRFIMCS RU-WRF has
been proven to be a
highly successful andtrusted tool in theprediction of day-to-day, severe, andoffshore weather.
RU-WRF has beenused to forecast day-to-day and severeweather conditionsfor PSEG for morethan seven years.The model has beenused foroceanographicprojects funded bythe Navy, NSF, etc.
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IMCS RU-WRF was the first operational weather model (US Gov. orotherwise) to accurately predict the path of Tropical Storm Ernesto
through the Middle-Atlantic States in 2006.
Operational Mesoscale Modelingwith RU-WRF
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Capability of Real-time Energy
Forecasts
Energy Yield Turbine by TurbineWake LossSevere Weather Outage
Tropical Storms Noreasters Thunderstorms/lightning Ice Accretion
Inaccessibility due to high seas and
winds Real-time Construction Climatological
Operational Mesoscale Modelingwith RU-WRF
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Wind Power
m/s
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Sea Breeze Development
RU-WRF Model SimulationInfrared Satellite
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Sea Breeze Development
Infrared Satellite RU-WRF Model Simulation
Neutral Case
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Sea Breeze Development
cation of Sea Breeze Front at 100 metersUpwelling SST Sea Breeze ~ 8.6 kmfarther west than Neutral Case SST
Upwelling SSTSea Breeze @ 100 m
74.05 W
Upwelling Case vs. Neutral Case SST
Vertical Cross-Section, 39.8 N
meters
Neutral SSTSea Breeze @ 100 m
73.95 W
Temperature CTemperature C
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NJ Sea Breeze Event
RU-WRF Model 2km Simulation
Wind Speed [m/s]
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NJ Sea Breeze Cross Section
kil
ome
ters
Wind Speed [m/s]
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Scope of Work Details
1. High resolution, microscale modelresolving sea breeze2. High resolution boundary conditions to
resolve upwelling centers
3. Map surface currents to confirm horizontalwind distributions at the microscale
4. Vertical validation from monitoring sites5. Run for a year over a sea breeze season to
populate database and calculate hourlystatistics by month
P d WRF d i
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2 km horizontal
resolution over NYBight 0.67 km horizontal
resolution over studyarea
Model will run inreal-time, for precisecomparison to onsitemet towers
Data will be extracted
from the model at anarray of grid points,representing locations5 miles, 10 miles, 15
miles,and 20 miles offshore at
10 mile intervalsnorthward
Proposed WRF domain
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Scope of Work Details
1. High resolution, microscale model resolvingsea breeze2. High resolution boundary conditions to
resolve upwelling centers
3. Map surface currents to confirm horizontalwind distributions at the microscale
4. Vertical validation from monitoring sites5. Run for a year over a sea breeze season to
populate database and calculate hourlystatistics by month
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ConditionsOuterboundary
conditions(incl. soil
moisture): highres. 4km NAM
LandUse:
USGS 24-category
SST: high res.1km 14-daycomposite
product (MODIS,etc.)
High res.,nested RU-
WRF: 10-20mnear surfacevertical res.
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Scope of Work Details
1. High resolution, microscale model resolvingsea breeze2. High resolution boundary conditions to
resolve upwelling centers
3. Map surface currents to confirmhorizontal wind distributions at themicroscale
4. Vertical validation from monitoring sites
5. Run for a year over a sea breeze season topopulate database and calculate hourlystatistics by month
Rutgers University - Coastal Ocean Observation Lab
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CODAR
Network
Glider
Fleet
L-Band & X-Band
Satellite Receivers
3-D Nowcasts
& Forecasts
Rutgers University - Coastal Ocean Observation LabObservatory Operations & Education Center
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MediumRange
Network
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CODAR Electronics Combined Transmit/Receive Anten
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Enhanced Hi resolution HF radar Coverage
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Enhanced Hi-resolution HF radar Coverage
Horizontal Resolution: 6 kmTemporal Average: 3 hoursHorizontal Resolution: 1 km
Temporal Average: 1 hour (or less)
HF Radar Derived Linear Wind Model
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Rotate wind vectors according to complex correlation
Calculate the slope and intercept of best fit line
U'c(x,y,t) = slope(x,y)*W'(t)
HF Radar Derived Linear Wind Model
Wind Transient [W'] (cm/s)
Cu
rrentTransient[U'](cm/s)
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Scope of Work Details
1. High resolution, microscale model resolvingsea breeze2. High resolution boundary conditions to
resolve upwelling centers
3. Map surface currents to confirm horizontalwind distributions at the microscale
4. Vertical validation from monitoringsites
5. Run for a year over a sea breeze season topopulate database and calculate hourlystatistics by month
Coastal/Offshore Monitoring
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Coastal/Offshore MonitoringMeteorological
TowerMeteorological Buoy Offshore vertical
LIDAR
Coastal/OffshoreScanning LIDAR
Infrared Satellite Coastal Radar(CODAR)
http://www.axystechnologies.com/LinkClick.aspx?link=136&tabid=68http://www.axystechnologies.com/LinkClick.aspx?link=136&tabid=68 -
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Scope of Work Details
1. High resolution, microscale model resolvingsea breeze2. High resolution boundary conditions to
resolve upwelling centers
3. Map surface currents to confirm horizontalwind distributions at the microscale
4. Vertical validation from monitoring sites5. Run for a year over a sea breeze season
to populate database and calculatehourly statistics by month
Virtual Meteorological Tower Output
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Virtual Meteorological Tower Outputat 48 locations
Example of wind speed (m/s) at tower12x24 January February March April May June July August Septemb
erOctober Novembe
rDecembe
r
2300-0000
6.83 7.22 7.67 5.74 7.01 6.5 5.55 5.93 5.81 6.79 6.78 7.23
2200-2300
6.78 7.39 7.5 5.83 7.07 6.32 6.15 5.56 6.3 6.72 6.68 6.68
2100-2200
6.66 7.3 7.02 6 6.66 6.02 6.34 5.63 6.05 6.49 6.66 6.86
2000-2100
6.44 7.15 6.93 5.85 6.36 5.65 6.41 5.62 6.01 6.36 6.5 6.7
1900-2000
6.4 6.93 6.73 5.49 6.08 5.52 5.69 5.27 5.71 6.48 6.67 7.02
1800-1900
6.18 7.14 6.62 5.58 6.22 5.55 5.32 4.83 5.48 6.36 6.22 7.31
1700-
1800
5.86 6.91 7.03 5.84 6.72 6.09 5.65 4.82 5.3 5.74 6.17 6.92
1600-1700
5.89 7.06 7.66 6.17 6.83 6.46 5.96 5.39 5.66 5.59 6.09 6.82
1500-1600
6.05 7.12 7.78 6.52 6.98 6.41 6.18 5.58 5.87 6.12 6.44 7.44
1400-1500
6.6 7.15 8.1 6.68 6.95 6.32 6.01 5.33 5.87 6.33 6.4 7.63
1300-1400
6.45 7.19 8.01 6.57 7.04 6 5.79 5.53 5.72 6.45 6.7 7.84
1200-1300
6.51 7.37 7.44 6.63 6.82 5.54 5.4 5.13 5.53 6.33 6.72 7.7
1100-1200 6.37 7.09 7.07 6.3 6.61 5.07 4.61 4.91 5.38 6.31 6.76 7.51
1000-1100
6.25 6.95 6.83 6.38 6.39 4.85 4.07 4.36 5.44 6.27 6.85 7.25
0900-1000
6.23 7.14 6.8 6.34 6.12 4.5 3.81 3.91 5.48 5.83 6.54 6.65
0800-0900
6.34 6.96 6.44 5.96 5.55 4.44 3.69 3.82 5.33 5.4 6.41 6.95
0700-0800
6.76 7.09 6.16 5.55 5.56 4.21 3.69 3.74 5.34 6.54 6.94 6.93
0600-0700
6.82 7.11 6.22 5.57 5.88 4.39 4.03 4.46 6.04 7.33 7.26 6.88
0500-0600
6.84 6.74 6.51 6.08 6.73 5.64 5.03 5.5 6.43 7.36 7.2 7.37
0400- 6.85 6.68 7.16 6.46 6.89 6.03 5.38 5.83 6.29 7.3 7.02 7.42
Virtual Meteorological Tower Output
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Virtual Meteorological Tower Outputat 48 locations
Example of wind speed (m/s) at tower
Wind Power Production (m3/s3)
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Wind Power Production (m /s )
Wind Speed Anomaly (m/s)
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Wind Speed Anomaly (m/s)
Wind Power Production Anomaly (m3/s3)
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Wind Power Production Anomaly (m /s )
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Deliverables
1. Weather analysis database2. Surface current database3. Validation study
a. Use our horizontal data plus OSW
developers vertical data4. Summary statistics
RU-WRF High-Resolution Wind
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Resource Analysis
Lines A-L spaced 10 nm apart, South/North along NJcoastline
Points along lines spaced 5 nm apart, West/East alongNJ coastline
Array 12 x 4 throughout the coastal waters out to 20nm
Wind climatology to be conducted at 48 Virtual Met
Tower locations
Results made available via GIS platform
10nm
5 nm
Meteorological Tower vs
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Meteorological Tower providesdata at instrumented heights at
a single location
Virtual Meteorological Towerprovides data any desired
height at any location
Meteorological Tower vs.Model Virtual Meteorological
Tower The Virtual MetTower can allowfor additionalvariables to becalculated suchas temperature,air density,turbulence,potential turbineicing, and bladeswept area windshear.
Virtual Meteorological Tower Output
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Virtual Meteorological Tower Outputat 48 locations
Wind speed data at anydesired height above the
water surface on hourly,daily, monthly, annual, andlong-term temporal scales.
Wind Speed Rose (blue) andEnergy Rose (red) Crucial for
determining turbine layout forenergy optimization and wakeimpact.
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k
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Tasks
1. Configure/set-up high res., nested RU-WRF
a. Optimize physics, microphysics schemes
b. Optimize boundary conditions (high res. SST, landuse, soil moisture)
2. Set-up, commence 13MHz CODAR network for
horizontal atmospheric model validation
3. Coordinate with BPU and developers for verticalatmospheric model validation
4. Run RU-WRF for a year with emphasis on seabreeze season which coincides with peakenergy demand
k
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Tasks
5. Vertical and horizontal validation of RU-WRFusing monitoring sites and CODAR network
6. Produce high-res, 3-D wind resource maps
7. Collaborate with NJDEP to help identify
optimum wind resource locations8. Provide operational weather forecasts in
support of wind power production potential andenergy market applications
P d Sit L ti
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Proposed Site Location North Wildwood
P d Sit L ti
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Proposed Site Location Strathmere
P d Sit L ti
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Proposed Site Location Brigantine
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RU-WRF to ROMS Coupling
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RU WRF to ROMS CouplingOur atmospheric model, RU-WRF, will be coupled to our ocean model, ROMS
(Regional Ocean Modeling System), to investigate the effects of coastalupwelling on sea breeze activity
ROMS SST and currents at200 m
RU-WRF Wind andSurface T
MARACOOS Regional Themes
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g
7 3 3 0 ' W
7 3 3 0 ' W
7 4 0 ' W
7 4 0 ' W
7 4 3 0 ' W
7 4 3 0 ' W
7 5 0 ' W
7 5 0 ' W
7 5 3 0 ' W
7 5 3 0 ' W
7 6 0 ' W
7 6 0 ' W
3
9
3
0
'N
3
9
3
0
'N
3
9
0
'N
3
9
0
'N
3
8
3
0
'N
3
8
3
0
'N
3
8
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'N
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0
'N
3
7
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A r e a s u n d e r C o n s i d e r a t i o n fo r W i n d E n e r g y A r e a s
N e w J e r s e y
D e l a w a r e
M a r y l a n d
V i r g i n i a
0 5 1 0 1 5 2 0 2 5 3 0
N a u t i c a l M i l e s
M a r y l a n d
N e w J e r s e y
D e l a w a r e
C H E S A P E A K E
B A Y
D E L A W A R E
B A Y
Vir
gi
ni a
V i r g i n i a
V i r g i n i aB e a c h
O c e a nC i t y
A t l a n t i cC i t y
D o v e r
W i l m i n g t o nP e n n s y l v a n i a
aritime Operations Safety at Sea
2) Ecosystem DecisionSupport - Fisheries
3) Water Quality Floatables, Hypoxia, Nutrient
4) Coastal Inundation - Flooding
5) Energy Offshore Wind
redications: New Jersey Observations and Models
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Observationsfocused onoptimizing forecastsoff the NJ Coast
Circulation Model
GNOME Oil Trajectories
NYHOPSStevens Institute of Technology
HF Radar Gliders
Water Monitoring& Standards
nomous Platforms: Dissolved OxygenNJDEP
EPA
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ygerra Optode
Oxygen Concentration
EPARutgers
MACOORA
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Conclusions
1. A high resolution, sea breeze-resolving atmosphericforecast model will be operated for 1 year to fullyencompass a winter storm and summer sea breezeseason
2. Improved boundary conditions from the 4km NAMand upwelling-resolving satellite SST will be used
3. A unique observing network will be deployed toprovide spatial validation data
4. An annual database will be developed andsummary statistics calculated