Atmospheric processes, such as wind, impact the ground motion of the earth and have the potential to induce strong broad-band noise in seismological records. In order to quantify the influence of wind on ground motion velocity joint seismological and meteorological measurements were conducted at the Dead Sea.
Results reveal a pronounced impact of wind on seismological records. A methodology is presented to account for the dependency of PSD of ground motion velocity on the horizontal wind field.
Umfang: VI, 247 S.
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Lott, F. 2017. Wind Systems in the Dead Sea and Footprints in Seismic Records. Karlsruhe: KIT Scientific Publishing. DOI: https://doi.org/10.5445/KSP/1000060565
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Veröffentlicht am 22. Februar 2017