13.07.2015 Views

TurbSim User's Guide: Version 1.06.00 - NREL

TurbSim User's Guide: Version 1.06.00 - NREL

TurbSim User's Guide: Version 1.06.00 - NREL

SHOW MORE
SHOW LESS

Create successful ePaper yourself

Turn your PDF publications into a flip-book with our unique Google optimized e-Paper software.

Figure 20. GPLLJ-model stable/neutral turbulence as a function of local stability and shearvelocitiesσv0.70 ≤ ≤ 0.98, (42)σuandσw0.52 ≤ ≤ 0.71. (43)σBy design, most of the LLLJP data was collected in the stable atmosphere. As a result, there wasnot enough data to create a model of the spectra in unstable flows. Instead, the GP_LLJ spectrafor unstable atmospheric conditions use the same equations as the SMOOTH model spectra inEq. (33) through Eq. (35). The one difference is that the GP_LLJ scales the spectra using thelocal u*values instead of the UStar input parameter. The GP_LLJ spectra for unstable flows arethus defined as2uu*SK( f ) = S2 K , SMOOTH ( f ) . (44)UStarWF_UPW: The <strong>NREL</strong> Wind Farm, Upwind ModelThe WF_UPW wind-farm model is based on measurements taken from a 50-m tower upwind ofa large wind plant in San Gorgonio Pass, California. The spectra were calculated using 50-Hzwind-speed measurements from a three-axis sonic anemometer located 23 m above the ground.The parameters for spatial coherence were calculated using measurements from 5-Hz cupanemometers and direction vanes located at 5 m, 10 m, 20 m and 50 m above ground level.Please refer to Kelley [5] for details of the model development and Kelley and Wright [31] forfurther details on the measurements.36

Hooray! Your file is uploaded and ready to be published.

Saved successfully!

Ooh no, something went wrong!