Webtopographic amplification factor. A ratio, calculated solely from topographic (terrain elevation) data, of the diurnal temperature amplitude or range in a valley to that at the same altitude over the adjacent plain. The diurnal amplitude is larger (or "amplified") over the valley than over the plain because the volume of air is less in the ... WebDec 1, 2024 · Considering topographic amplification is particularly important for seismic design in mountainous regions like Hong Kong. Due to its complexity, topographic amplification has not yet been considered in most seismic design codes, with only a few exceptions such as the Eurocode 8, the 1995 France seismic code and the 2010 Chinese …
On the role of topographic amplification in seismic slope instabilities ...
WebMay 17, 2024 · The discrepancy possibly reflects the amplification of subsidence due to selective deployment of the GNSS stations in concave terrains Plain Language Summary … WebThe seismic topographic effect is one of the debated research topics in seismology and earthquake engineering. This debate is due to the discrepancy between the observed amplification and the amplification underestimation in numerical simulations. Although the numerical simulation of ground motion, which began in the 1970s, has been an important … setzer airship
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WebMay 17, 2024 · A tropical cyclone transports a large amount of sea water to land as water vapor. The water becomes a torrential downpour, and the rainwater temporarily staying on land depresses the solid earth as a load. WebMar 14, 2024 · @article{osti_1358161, title = {An experimental topographic amplification study at Los Alamos National Laboratory using ambient vibrations}, author = {Stolte, Andrew C. and Cox, Brady R. and Lee, Richard C.}, abstractNote = {An experimental study aimed at investigating potential topographic amplification of seismic waves was conducted on a … WebJul 7, 2024 · Previous studies, using displacement, acceleration and acceleration response spectra, reported topographic seismic amplification factors between 2 and 75 per cent, and found that amplification generally occurs at the slopes and at the top of topographic features whereas deamplification occurs at the bottom of slopes (e.g. Boore 1972; … the torridon inverness