Three Peaks of 2011 Draconid Activity Including that Connected with Pre-1900 Material
Identifikátory výsledku
Kód výsledku v IS VaVaI
<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F67985815%3A_____%2F14%3A00433643" target="_blank" >RIV/67985815:_____/14:00433643 - isvavai.cz</a>
Výsledek na webu
<a href="http://dx.doi.org/10.1007/s11038-014-9435-9" target="_blank" >http://dx.doi.org/10.1007/s11038-014-9435-9</a>
DOI - Digital Object Identifier
<a href="http://dx.doi.org/10.1007/s11038-014-9435-9" target="_blank" >10.1007/s11038-014-9435-9</a>
Alternativní jazyky
Jazyk výsledku
angličtina
Název v původním jazyce
Three Peaks of 2011 Draconid Activity Including that Connected with Pre-1900 Material
Popis výsledku v původním jazyce
A Draconid meteor shower outburst was observed from on board two scientific aircraft deployed above Northern Europe on 8th October 2011. The activity profile was measured using a set of photographic and video cameras. The corrected hourly rates reached avalue of almost 350. The brighter meteors peaked about 15-20 min earlier than the dimmer ones. This difference can be explained by different directions of the ejection of the meteoroids from the parent comet. One of the instruments was even able to detect meteors connected with the material ejected from the parent comet before 1900 and thus confirmed the prediction of the model, although it was based on uncertain pre-1900 cometary data. Another small peak of the activity, which was caused by material ejected during the 1926 perihelion passage of the parent comet, was detected around 21:10 UT. The mass distribution index determined using the narrow field-of-view video camera was 2.0 +/- A 0.1. This work shows that the observation of met
Název v anglickém jazyce
Three Peaks of 2011 Draconid Activity Including that Connected with Pre-1900 Material
Popis výsledku anglicky
A Draconid meteor shower outburst was observed from on board two scientific aircraft deployed above Northern Europe on 8th October 2011. The activity profile was measured using a set of photographic and video cameras. The corrected hourly rates reached avalue of almost 350. The brighter meteors peaked about 15-20 min earlier than the dimmer ones. This difference can be explained by different directions of the ejection of the meteoroids from the parent comet. One of the instruments was even able to detect meteors connected with the material ejected from the parent comet before 1900 and thus confirmed the prediction of the model, although it was based on uncertain pre-1900 cometary data. Another small peak of the activity, which was caused by material ejected during the 1926 perihelion passage of the parent comet, was detected around 21:10 UT. The mass distribution index determined using the narrow field-of-view video camera was 2.0 +/- A 0.1. This work shows that the observation of met
Klasifikace
Druh
J<sub>x</sub> - Nezařazeno - Článek v odborném periodiku (Jimp, Jsc a Jost)
CEP obor
BN - Astronomie a nebeská mechanika, astrofyzika
OECD FORD obor
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Návaznosti výsledku
Projekt
Výsledek vznikl pri realizaci vícero projektů. Více informací v záložce Projekty.
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
Údaje specifické pro druh výsledku
Název periodika
Earth, Moon, and Planets
ISSN
0167-9295
e-ISSN
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Svazek periodika
112
Číslo periodika v rámci svazku
1-4
Stát vydavatele periodika
NL - Nizozemsko
Počet stran výsledku
17
Strana od-do
15-31
Kód UT WoS článku
000339720000003
EID výsledku v databázi Scopus
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