Poslední pokroky a obtíže ve zkoumání infrazvukových vln v ionosféře

Kód výsledku v IS VaVaI

<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F68378289%3A_____%2F06%3A00039196" target="_blank" >RIV/68378289:_____/06:00039196 - isvavai.cz</a>

Výsledek na webu

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DOI - Digital Object Identifier

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Jazyk výsledku

angličtina

Název v původním jazyce

RECENT ADVANCES AND DIFFICULTIES OF INFRASONIC WAVE INVESTIGATION IN THE IONOSPHERE

Popis výsledku v původním jazyce

Infrasonic waves have a remarkable ability to transfer energy from the ground up to the uppermost layers of the atmosphere, because they carry the major part of their energy upwards through the atmosphere. The only opportunity to monitor propagation of an infrasonic wave at high altitudes is to watch for its influence on the ionospheric plasma using the Doppler method of radiosounding of the ionosphere. The ionospheric method for sensing aboveground and underground explosions has been developed. Its main advantage is the remote observation of an explosion in the near-field zone by means of short radio waves, i.e., the radio sounding of the ionosphere directly above the explosion. The theory of propagation of an acoustic pulse produced by an explosion on the ground up to ionospheric heights has been developed better than the theory for other sources, and has been quantitatively confirmed by experiments.

Název v anglickém jazyce

RECENT ADVANCES AND DIFFICULTIES OF INFRASONIC WAVE INVESTIGATION IN THE IONOSPHERE

Popis výsledku anglicky

Infrasonic waves have a remarkable ability to transfer energy from the ground up to the uppermost layers of the atmosphere, because they carry the major part of their energy upwards through the atmosphere. The only opportunity to monitor propagation of an infrasonic wave at high altitudes is to watch for its influence on the ionospheric plasma using the Doppler method of radiosounding of the ionosphere. The ionospheric method for sensing aboveground and underground explosions has been developed. Its main advantage is the remote observation of an explosion in the near-field zone by means of short radio waves, i.e., the radio sounding of the ionosphere directly above the explosion. The theory of propagation of an acoustic pulse produced by an explosion on the ground up to ionospheric heights has been developed better than the theory for other sources, and has been quantitatively confirmed by experiments.

Druh

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

CEP obor

DG - Vědy o atmosféře, meteorologie

OECD FORD obor

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Projekt

<a href="/cs/project/GA205%2F04%2F2110" target="_blank" >GA205/04/2110: Efekty infrazvukových vln na ionosféru</a><br>

Návaznosti

Z - Vyzkumny zamer (s odkazem do CEZ)

Rok uplatnění

2006

Kód důvěrnosti údajů

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

Název periodika

Surveys in Geophysics

ISSN

0169-3298

e-ISSN

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Svazek periodika

27

Číslo periodika v rámci svazku

2

Stát vydavatele periodika

NL - Nizozemsko

Počet stran výsledku

41

Strana od-do

169-209

Kód UT WoS článku

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EID výsledku v databázi Scopus

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