Alternative Mechanisms of the Microseisms Excitation
Identifikátory výsledku
Kód výsledku v IS VaVaI
<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F68145535%3A_____%2F14%3A00435072" target="_blank" >RIV/68145535:_____/14:00435072 - isvavai.cz</a>
Nalezeny alternativní kódy
RIV/67985891:_____/14:00435072 RIV/47813059:19810/14:#0000003
Výsledek na webu
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DOI - Digital Object Identifier
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Alternativní jazyky
Jazyk výsledku
angličtina
Název v původním jazyce
Alternative Mechanisms of the Microseisms Excitation
Popis výsledku v původním jazyce
The annual drift is typical for microseisms. We propose a model based on the generation of thermoelastic waves, which explains the highest microseisms during winter by the higher stress level. If we remove the average influence of the stress background from the microseisms, we obtain the residua of microseisms, which show the semiannual periods with the maxima in March and October. The histogram of occurrence of anomalous microseisms has the same form as the variations of Length Of the Day (LOD). This mechanism was recognized as a secondary order mechanism after the annual drift. The synoptic situations and earthquakes were recognized as imminent triggers of anomalous microseisms. This synoptic situation is consistent with the uplift of the northern part of Europe after the ice cup melting.
Název v anglickém jazyce
Alternative Mechanisms of the Microseisms Excitation
Popis výsledku anglicky
The annual drift is typical for microseisms. We propose a model based on the generation of thermoelastic waves, which explains the highest microseisms during winter by the higher stress level. If we remove the average influence of the stress background from the microseisms, we obtain the residua of microseisms, which show the semiannual periods with the maxima in March and October. The histogram of occurrence of anomalous microseisms has the same form as the variations of Length Of the Day (LOD). This mechanism was recognized as a secondary order mechanism after the annual drift. The synoptic situations and earthquakes were recognized as imminent triggers of anomalous microseisms. This synoptic situation is consistent with the uplift of the northern part of Europe after the ice cup melting.
Klasifikace
Druh
O - Ostatní výsledky
CEP obor
DC - Seismologie, vulkanologie a struktura Země
OECD FORD obor
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Návaznosti výsledku
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
Ostatní
Rok uplatnění
2014
Kód důvěrnosti údajů
S - Úplné a pravdivé údaje o projektu nepodléhají ochraně podle zvláštních právních předpisů