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Preliminary assessment of wind climate fluctuations and use of Dynamical Systems Theory for resource assessment. Wolf-Gerrit Früh Christina Skittides With support from SgurrEnergy. Questions. How sensitive is the electricity production of a wind farm to the local wind statistics

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Presentation Transcript
slide1
Preliminary assessment of wind climate fluctuations and use of Dynamical Systems Theory for resource assessment

Wolf-Gerrit Früh

Christina Skittides

With support from SgurrEnergy

questions
Questions
  • How sensitive is the electricity production of a wind farm to the local wind statistics
  • How will climate change affect the electricity production from wind farms?
  • How large are inter-annual variations in the electricity production due to weather fluctuations?
  • How much can a large spatial distribution of wind farms smooth electricity output
  • Can we use dynamic information for an improved wind resource assessment and prediction at potential development sites?
data used
Data used
  • Land surface wind data from the MIDAS data record provided by the British Atmospheric Data Centre, maintained by NERC
    • Hourly winds from weather stations all over the UK
    • In particular from two stations in Edinburgh, Gogarbank and Blackford Hill
    • Data format
      • Wind speed in knots at 10 m above sea level
      • Wind direction in degrees
  • Wind data converted to m/s at a typical turbine hub
assumptions
Assumptions
  • Standard wind shear profile
  • Best-fit Weibull distribution
  • Typical turbine performance curve
  • Ideal turbine response
  • All generation exported for use
from wind distribution to electricity
From wind distribution to electricity
  • Number of hours during which the wind was u: Φ(u) * T
  • The output from a turbine during that time: P(u)
  • The electricity generated during those hours: E(u)= P(u) * Φ(u) * T
  • Total output:Etotal= ΣE(u)
weibull and rayleigh distributions
Weibull and Rayleigh distributions
  • Cumulative Weibull
    • k: shape factor
  • Weibull
    • c: scale factor
sensitivity analysis
Sensitivity analysis

6

5

4

3

2

Example:

100 MW farm with expected

Capacity factor 30%: Income £26.2 m

Actual Capacity factor 27%: Income £23.6 m

Deficit: £ 2.4 m

does the wind always blow somewhere
Does the wind always blow somewhere?

Fraction of sites not producing

Fraction of sites producing at part capacity

Fraction of sites producing at full capacity

has the wind changed
Has the wind changed?

Edinburgh Gogarbank

Ccap = 0.14 ± 0.06

has the wind changed1
Has the wind changed?

Edinburgh Blackford Hill

Ccap = 0.28 ± 0.08

assessing resource from a short measurement campaign
Assessing resource from a short measurement campaign
  • Short time to measure potential site
    • Does not give good statistics
  • Are the measurements correlated to a site nearby with existing longer record?
  •  Use ‘MCP’
    • Measure a short record
    • Correlate with longer record
    • Predict resource at location with shorter record
  • Christina
statistical modelling of wind energy resource

Statistical Modelling of Wind Energy Resource

Christina Skittides

Supervisor: Dr. Wolf G. Früh

17th March 2011

mcp methods
MCP Methods
  • MCP goal: characterize wind speed distribution and estimate the annual energy capture of a wind farm
  • MCP methods: model relationship between wind speed and direction at two sites
    • Measurement period: a year or more
    • Input: wind speed and wind direction
    • Output: mapping from one site to other
    • Use: apply mapping to more data from reference site
mcp methods1
MCP Methods
  • MCP invariants:
    • wind speed, direction
    • distance, eg. time of flight delays
    • effects of terrain on the flow, eg. local obstructions
    • large/small–scale weather, eg. atmospheric stability
dynamical systems theory
Dynamical Systems Theory
  • Dynamical systems involve differential equations that depend on position and momentum
  • Phase space: describes the system’s variables
  • Attractor: defines the solution of the system
  • Orbit: the path the system follows during its evolution

Method needed to define equivalent variables to the phase space ones Time-delay

time delay pca theory
Time-Delay/PCA Theory

Time-Delay:

  • practical implementation of dynamical systems
  • Results sensitive to choice of delays PCA

PCA:

  • non-parametric method to optimize phase space reconstruction
  • identifies number of needed time- delays
  • gives picture of their shape
  • reduces dimensions so as to extract useful information
pca theory
PCA theory

Useful PCA outputs:

  • Singular Vectors: represent the dimensions of the phase space, describe optimum way of reconstructing it
  • Singular Values: measure total contribution of each dimension to total variance
  • Principal Components (PC): describe the system’s time series, separate important variables from noise
pendulum example
Pendulum Example
  • Dynamical system with two inputs x,y
    • Case A (without noise):

x= 3sin(t/0.7)

y= x+0.4sin(t/π)

    • Case B (with noise):

x= 3sin(t/0.7)

y= x+0.4sin(t/π) + 0.6ε

conclusions
Conclusions
  • PCA is robust and useful for time series of multiple inputs
  • Noisy or “clean”data: no significant differences
  • Choice of time-delay length and gap of entries in the matrix not important
gogarbank data
Gogarbank Data
  • 10 year (2000-2010) data taken from Gogarbank station, Edinburgh
  • Input variables: wind speed, direction, pressure, temperature
  • Apply PCA to different models:
    • all variables
    • wind speed, direction and pressure
    • only wind speed and direction
gogarbank data1
Gogarbank Data
  • Only wind speed and direction,hourly measurements per week
conclusions1
Conclusions
  • Gogarbank station wind: dynamic behaviour found in structure of PCs and singular vectors
  • Adding pressure no significant difference
  • Temperature changes results significantly since PCs concentrate on seasonal cycle
  • Cyclic behaviour over the year, more windy around January and from September- December
  • Using 1 week or 2 weeks identifies weather (typical predictability of weather ~ 14 days)
following steps
Following Steps
  • Apply PCA to simultaneous data from two weather stations (Gogarbank & Blackford Hill, Edinburgh)
    • Application to a one-year segment
    • Using Gogarbank for other years to predict Blackford Hill
    • Comparison with actual measurements from Blackford Hill
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