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  • The basic scientific question of this study was: do other mechanisms exist for excitation of secondary microseisms aside from the widely accepted mechanism by non-linear interactions of respective ocean waves. Here we use continuous broad- band data from secondary microseisms recorded at the Ostrava-Krásné Pole, Czech Republic (OKC) seismic station to create a massive seismological database. Except for seismological data, various meteorological features and their mutual relations were analysed: temperature, the so called “shifted temperature, air density, changes of atmospheric pressure, and synoptic situations. These analyses prove that maximum amplitudes of microseisms were observed during winter, while minimum amplitudes occured in summer months. The annual variations of microseisms amplitudes could not be explained by annual variations of storm activity above the North Atlantic. In addition, current analyses also aim at quantitative and quantitative evaluation of synoptic situations for triggering individual microseismic anomalies.
  • The basic scientific question of this study was: do other mechanisms exist for excitation of secondary microseisms aside from the widely accepted mechanism by non-linear interactions of respective ocean waves. Here we use continuous broad- band data from secondary microseisms recorded at the Ostrava-Krásné Pole, Czech Republic (OKC) seismic station to create a massive seismological database. Except for seismological data, various meteorological features and their mutual relations were analysed: temperature, the so called “shifted temperature, air density, changes of atmospheric pressure, and synoptic situations. These analyses prove that maximum amplitudes of microseisms were observed during winter, while minimum amplitudes occured in summer months. The annual variations of microseisms amplitudes could not be explained by annual variations of storm activity above the North Atlantic. In addition, current analyses also aim at quantitative and quantitative evaluation of synoptic situations for triggering individual microseismic anomalies. (en)
Title
  • Mutual Coupling Between Meteorological Parameters and Secondary Microseisms
  • Mutual Coupling Between Meteorological Parameters and Secondary Microseisms (en)
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  • Mutual Coupling Between Meteorological Parameters and Secondary Microseisms
  • Mutual Coupling Between Meteorological Parameters and Secondary Microseisms (en)
skos:notation
  • RIV/68145535:_____/13:00420828!RIV14-MSM-68145535
http://linked.open...avai/riv/aktivita
http://linked.open...avai/riv/aktivity
  • I, P(LM2010008)
http://linked.open...iv/cisloPeriodika
  • 6
http://linked.open...vai/riv/dodaniDat
http://linked.open...aciTvurceVysledku
http://linked.open.../riv/druhVysledku
http://linked.open...iv/duvernostUdaju
http://linked.open...titaPredkladatele
http://linked.open...dnocenehoVysledku
  • 90246
http://linked.open...ai/riv/idVysledku
  • RIV/68145535:_____/13:00420828
http://linked.open...riv/jazykVysledku
http://linked.open.../riv/klicovaSlova
  • secondary microseisms; meteorological elements; statistics (en)
http://linked.open.../riv/klicoveSlovo
http://linked.open...odStatuVydavatele
  • CN - Čínská lidová republika
http://linked.open...ontrolniKodProRIV
  • [0B548778EBA0]
http://linked.open...i/riv/nazevZdroje
  • Terrestrial Atmospheric and Oceanic Sciences
http://linked.open...in/vavai/riv/obor
http://linked.open...ichTvurcuVysledku
http://linked.open...cetTvurcuVysledku
http://linked.open...vavai/riv/projekt
http://linked.open...UplatneniVysledku
http://linked.open...v/svazekPeriodika
  • 24
http://linked.open...iv/tvurceVysledku
  • Kalenda, Pavel
  • Holub, Karel
  • Rušajová, Jana
http://linked.open...ain/vavai/riv/wos
  • 000329895100001
issn
  • 1017-0839
number of pages
http://bibframe.org/vocab/doi
  • 10.3319/TAO.2013.07.04.01(T)
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