Mutual Coupling Between Meteorological Parameters and Secondary Microseisms

Kód výsledku v IS VaVaI

<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F68145535%3A_____%2F13%3A00420828" target="_blank" >RIV/68145535:_____/13:00420828 - isvavai.cz</a>

Nalezeny alternativní kódy

RIV/67985891:_____/13:00420828

Výsledek na webu

<a href="http://tao.cgu.org.tw/pdf/v246p933.pdf" target="_blank" >http://tao.cgu.org.tw/pdf/v246p933.pdf</a>

DOI - Digital Object Identifier

<a href="http://dx.doi.org/10.3319/TAO.2013.07.04.01(T)" target="_blank" >10.3319/TAO.2013.07.04.01(T)</a>

Jazyk výsledku

angličtina

Název v původním jazyce

Mutual Coupling Between Meteorological Parameters and Secondary Microseisms

Popis výsledku v původním jazyce

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 fromsecondary 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 situation

Název v anglickém jazyce

Mutual Coupling Between Meteorological Parameters and Secondary Microseisms

Popis výsledku anglicky

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 fromsecondary 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 situation

Druh

J_x - Nezařazeno - Článek v odborném periodiku (Jimp, Jsc a Jost)

CEP obor

DC - Seismologie, vulkanologie a struktura Země

OECD FORD obor

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Projekt

<a href="/cs/project/LM2010008" target="_blank" >LM2010008: CzechGeo/EPOS ? Distribuovaný systém observatorních a terénních měření geofyzikálních polí v České republice</a><br>

Návaznosti

I - Institucionalni podpora na dlouhodoby koncepcni rozvoj vyzkumne organizace

Rok uplatnění

2013

Kód důvěrnosti údajů

S - Úplné a pravdivé údaje o projektu nepodléhají ochraně podle zvláštních právních předpisů

Název periodika

Terrestrial Atmospheric and Oceanic Sciences

ISSN

1017-0839

e-ISSN

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Svazek periodika

24

Číslo periodika v rámci svazku

6

Stát vydavatele periodika

CN - Čínská lidová republika

Počet stran výsledku

17

Strana od-do

933-949

Kód UT WoS článku

000329895100001

EID výsledku v databázi Scopus

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