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Statements

Subject Item
n2:RIV%2F68145535%3A_____%2F13%3A00420828%21RIV14-MSM-68145535
rdf:type
n4:Vysledek skos:Concept
rdfs:seeAlso
http://tao.cgu.org.tw/pdf/v246p933.pdf
dcterms:description
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.
dcterms:title
Mutual Coupling Between Meteorological Parameters and Secondary Microseisms Mutual Coupling Between Meteorological Parameters and Secondary Microseisms
skos:prefLabel
Mutual Coupling Between Meteorological Parameters and Secondary Microseisms Mutual Coupling Between Meteorological Parameters and Secondary Microseisms
skos:notation
RIV/68145535:_____/13:00420828!RIV14-MSM-68145535
n4:predkladatel
n20:ico%3A68145535
n5:aktivita
n9:I n9:P
n5:aktivity
I, P(LM2010008)
n5:cisloPeriodika
6
n5:dodaniDat
n15:2014
n5:domaciTvurceVysledku
n11:6762735 n11:3546233
n5:druhVysledku
n13:J
n5:duvernostUdaju
n14:S
n5:entitaPredkladatele
n10:predkladatel
n5:idSjednocenehoVysledku
90246
n5:idVysledku
RIV/68145535:_____/13:00420828
n5:jazykVysledku
n19:eng
n5:klicovaSlova
secondary microseisms; meteorological elements; statistics
n5:klicoveSlovo
n7:meteorological%20elements n7:statistics n7:secondary%20microseisms
n5:kodStatuVydavatele
CN - Čínská lidová republika
n5:kontrolniKodProRIV
[0B548778EBA0]
n5:nazevZdroje
Terrestrial Atmospheric and Oceanic Sciences
n5:obor
n6:DC
n5:pocetDomacichTvurcuVysledku
2
n5:pocetTvurcuVysledku
3
n5:projekt
n18:LM2010008
n5:rokUplatneniVysledku
n15:2013
n5:svazekPeriodika
24
n5:tvurceVysledku
Kalenda, Pavel Rušajová, Jana Holub, Karel
n5:wos
000329895100001
s:issn
1017-0839
s:numberOfPages
17
n16:doi
10.3319/TAO.2013.07.04.01(T)