Thunderstorm ? lower ionosphere relationship as shown by ionograms recorded at Pruhonice in two summer campaigns of 2013

Kód výsledku v IS VaVaI

<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F68378289%3A_____%2F14%3A00436773" target="_blank" >RIV/68378289:_____/14:00436773 - 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

Thunderstorm ? lower ionosphere relationship as shown by ionograms recorded at Pruhonice in two summer campaigns of 2013

Popis výsledku v původním jazyce

Thunderstorm ? ionosphere coupling have been studied by ionograms obtained from the Digisonde DPS4D at Pruhonice, Czech Republic and using a five-point continuous Doppler sounding system operating at 3.59 MHz during two campaigns in summer, 2013. Thunderstorms passed through the Czech Republic on 29th of May (09:50 - 15:25) and on 20th of June (18:00 - 24:00). The corresponding lightning activity was recorded by the LINET and BlitzOrtung lightning detection networks. In the second case, numerous spriteswere captured above the thunderstorm in the region of the ionosonde from Sopron, Hungary. During that period, ionograms were recorded in every minute. Peaks of ionospheric fmin values occurred much more frequently and with higher amplitudes characteristically in the period of sprites occurrences. Moreover the lack of the sporadic E layer has been found in those hours.

Název v anglickém jazyce

Thunderstorm ? lower ionosphere relationship as shown by ionograms recorded at Pruhonice in two summer campaigns of 2013

Popis výsledku anglicky

Thunderstorm ? ionosphere coupling have been studied by ionograms obtained from the Digisonde DPS4D at Pruhonice, Czech Republic and using a five-point continuous Doppler sounding system operating at 3.59 MHz during two campaigns in summer, 2013. Thunderstorms passed through the Czech Republic on 29th of May (09:50 - 15:25) and on 20th of June (18:00 - 24:00). The corresponding lightning activity was recorded by the LINET and BlitzOrtung lightning detection networks. In the second case, numerous spriteswere captured above the thunderstorm in the region of the ionosonde from Sopron, Hungary. During that period, ionograms were recorded in every minute. Peaks of ionospheric fmin values occurred much more frequently and with higher amplitudes characteristically in the period of sprites occurrences. Moreover the lack of the sporadic E layer has been found in those hours.

Druh

O - Ostatní výsledky

CEP obor

DG - Vědy o atmosféře, meteorologie

OECD FORD obor

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Projekt

<a href="/cs/project/GAP209%2F12%2F2440" target="_blank" >GAP209/12/2440: Dynamické vazby troposféra-ionosféra a jejich vliv na ionosférickou variabilitu</a><br>

Návaznosti

I - Institucionalni podpora na dlouhodoby koncepcni rozvoj vyzkumne organizace

Rok uplatnění

2014

Kód důvěrnosti údajů

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