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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

    0

    'N

    3

    8

    0

    'N

    3

    7

    3

    0

    'N

    3

    7

    3

    0

    'N

    3

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    0

    'N

    3

    7

    0

    'N

    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