A review of results of the international ionospheric Doppler sounder network
Identifikátory výsledku
Kód výsledku v IS VaVaI
<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F68378289%3A_____%2F17%3A00478392" target="_blank" >RIV/68378289:_____/17:00478392 - isvavai.cz</a>
Výsledek na webu
<a href="http://dx.doi.org/10.1016/j.asr.2017.01.032" target="_blank" >http://dx.doi.org/10.1016/j.asr.2017.01.032</a>
DOI - Digital Object Identifier
<a href="http://dx.doi.org/10.1016/j.asr.2017.01.032" target="_blank" >10.1016/j.asr.2017.01.032</a>
Alternativní jazyky
Jazyk výsledku
angličtina
Název v původním jazyce
A review of results of the international ionospheric Doppler sounder network
Popis výsledku v původním jazyce
This paper summarizes main recent results reached by the Czech-lead international network of ionospheric Doppler shift sounders.nThe network consists of Doppler sounders in the western half of Czechia (5 measuring paths, 3 frequencies with central receivers in Prague),nnorthern Taiwan (3 transmitters, two separated receivers, 1 frequency), and two similar systems (3 measuring paths with 1 receivernand 1 frequency) in Tucuman (north-western Argentina) and Hermanus (the southernmost South Africa). Main areas of research havenbeen: (1) propagation of gravity waves (2) ionospheric effects of earthquakes (3) low latitude/equatorial phenomena (4) ionosphericnresponse to strong meteorological phenomena (5) effects of solar flares, geomagnetic activity and geomagnetic micropulsations. Mainnresults: (1) Theoretically expected dominance of gravity wave propagation against wind has been confirmed. (2) Impact of a train of seismicnwaves (P, S, SS, Rayleigh) generated by the Tohoku 2011 M9.0 earthquake was registered in the ionosphere over the Czech Republicnas long-period infrasound at the distance of about 9000 km from epicenter. (3) Analysis of ionospheric infrasound excited by the Nepaln2015 M7.8 earthquake observed by the Czech and Taiwan Doppler sounders showed that the intensity of ionospheric signal is signifi-ncantly height and latitude dependent. Air/plasma compression has to be considered to compute air particle velocities from the observednDoppler shift. (4) Nonlinear effects result in formation of N-shaped pulse disturbance in the upper atmosphere/ionosphere above strongnearthquakes as was documented by the example of the M8.3 Illapel 2016 earthquake. (5) Spread F structures observed by Doppler soundersnin Tucuman and Taiwan (both under the crest of equatorial ionization anomaly) provide results consistent with S4 scintillation datanand with previous optical, GPS and satellite
Název v anglickém jazyce
A review of results of the international ionospheric Doppler sounder network
Popis výsledku anglicky
This paper summarizes main recent results reached by the Czech-lead international network of ionospheric Doppler shift sounders.nThe network consists of Doppler sounders in the western half of Czechia (5 measuring paths, 3 frequencies with central receivers in Prague),nnorthern Taiwan (3 transmitters, two separated receivers, 1 frequency), and two similar systems (3 measuring paths with 1 receivernand 1 frequency) in Tucuman (north-western Argentina) and Hermanus (the southernmost South Africa). Main areas of research havenbeen: (1) propagation of gravity waves (2) ionospheric effects of earthquakes (3) low latitude/equatorial phenomena (4) ionosphericnresponse to strong meteorological phenomena (5) effects of solar flares, geomagnetic activity and geomagnetic micropulsations. Mainnresults: (1) Theoretically expected dominance of gravity wave propagation against wind has been confirmed. (2) Impact of a train of seismicnwaves (P, S, SS, Rayleigh) generated by the Tohoku 2011 M9.0 earthquake was registered in the ionosphere over the Czech Republicnas long-period infrasound at the distance of about 9000 km from epicenter. (3) Analysis of ionospheric infrasound excited by the Nepaln2015 M7.8 earthquake observed by the Czech and Taiwan Doppler sounders showed that the intensity of ionospheric signal is signifi-ncantly height and latitude dependent. Air/plasma compression has to be considered to compute air particle velocities from the observednDoppler shift. (4) Nonlinear effects result in formation of N-shaped pulse disturbance in the upper atmosphere/ionosphere above strongnearthquakes as was documented by the example of the M8.3 Illapel 2016 earthquake. (5) Spread F structures observed by Doppler soundersnin Tucuman and Taiwan (both under the crest of equatorial ionization anomaly) provide results consistent with S4 scintillation datanand with previous optical, GPS and satellite
Klasifikace
Druh
J<sub>imp</sub> - Článek v periodiku v databázi Web of Science
CEP obor
—
OECD FORD obor
10509 - Meteorology and atmospheric sciences
Návaznosti výsledku
Projekt
<a href="/cs/project/GC15-07281J" target="_blank" >GC15-07281J: Jevy spojující neutrální a ionizovanou atmosféru</a><br>
Návaznosti
P - Projekt vyzkumu a vyvoje financovany z verejnych zdroju (s odkazem do CEP)
Ostatní
Rok uplatnění
2017
Kód důvěrnosti údajů
S - Úplné a pravdivé údaje o projektu nepodléhají ochraně podle zvláštních právních předpisů
Údaje specifické pro druh výsledku
Název periodika
Advances in Space Research
ISSN
0273-1177
e-ISSN
—
Svazek periodika
60
Číslo periodika v rámci svazku
8
Stát vydavatele periodika
GB - Spojené království Velké Británie a Severního Irska
Počet stran výsledku
15
Strana od-do
1629-1643
Kód UT WoS článku
000412620000006
EID výsledku v databázi Scopus
2-s2.0-85012280115