Figure 3.
Peak ground velocity (PGV) maps without (a) and with (b) topography and the resulting map of the amplification due to topography (c) for a single WT at the centre of the Weilrod WF showing that the amplitude increases at the permanent station (TNS). The amplitudes in (a) and (b) are normalized to the maximum amplitude in Fig. 4c (with 7 WTs), to compare the radiation of a single and multiple WTs. Note: The contour lines in (c) are representative of the digital elevation model.