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Wind Energy

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16<br />

Short Time Prediction of <strong>Wind</strong> Speeds<br />

from Local Measurements<br />

Holger Kantz, Detlef Holstein, Mario Ragwitz, Nikolay K. Vitanov<br />

Summary. We compare different schemes for the short time (few seconds) prediction<br />

of local wind speeds in terms of their performance. Special emphasis is laid on<br />

the prediction of turbulent gusts, where data driven continuous state Markov chains<br />

turn out to be quite successful. A test of their performance by ROC statistics is<br />

discussed in detail. Taking into account correlations of several measurement positions<br />

in space enhances the predictability. As a striking result, stronger wind gusts<br />

possess a better predictability.<br />

16.1 <strong>Wind</strong> Speed Predictions<br />

Whereas the three dimensional velocity field of the air in the atmosphere<br />

can be supposed to be described by the deterministic Navier–Stokes equations,<br />

possibly augmented by equations for the temperature and humidity<br />

(and hence density of the air) and with suitable boundary conditions, a local<br />

measurement yields data which appear to be random. In fact, deterministic behaviour<br />

of the local velocities is very unprobable, since (a) the Navier–Stokes<br />

equations contain already non-local interactions through the self-generated<br />

pressure field, and (b) the local wind speed changes due to the drift of the<br />

global wind field across the measurement position.<br />

Data analysis of wind speed recordings yields results which are fully consistent<br />

with stochastic data. We use time series recorded in Lammefjord by<br />

the Risø research centre [1]. These data are obtained from cup anemometers<br />

mounted on measurement masts at heights of 10, 20, and 30 m above ground,<br />

taken with 8 Hz sampling rate. The data sets report the absolute values of the<br />

wind speeds in the x–y-plane, together with the angle of incidence. In total,<br />

we use 10 days of data. Due to the non-stationarity of the data, the autocorrelation<br />

function cannot be reliably determined. In any case, correlations of<br />

the wind speed decay slowly, whereas the increments, i.e. the differences of succesive<br />

measurements, seem to be uncorrelated. Histograms of the differences<br />

vt − ¯vt of the data and the moving 1-minute mean velocities ¯vt, conditioned<br />

to the value of ¯vt, show an almost Gaussian behaviour with variances which

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