Statistical Characteristics of Ionospheric Hiss Waves
Identifikátory výsledku
Kód výsledku v IS VaVaI
<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F68378289%3A_____%2F19%3A00507763" target="_blank" >RIV/68378289:_____/19:00507763 - isvavai.cz</a>
Nalezeny alternativní kódy
RIV/00216208:11320/19:10407571
Výsledek na webu
<a href="http://nora.nerc.ac.uk/id/eprint/523674/1/Xia_et_al-2019-Geophysical_Research_Letters.pdf" target="_blank" >http://nora.nerc.ac.uk/id/eprint/523674/1/Xia_et_al-2019-Geophysical_Research_Letters.pdf</a>
DOI - Digital Object Identifier
<a href="http://dx.doi.org/10.1029/2019GL083275" target="_blank" >10.1029/2019GL083275</a>
Alternativní jazyky
Jazyk výsledku
angličtina
Název v původním jazyce
Statistical Characteristics of Ionospheric Hiss Waves
Popis výsledku v původním jazyce
In this study, we use the observations of electromagnetic waves by Detection of Electromagnetic Emissions Transmitted from Earthquake Regions satellite to investigate propagation characteristics of low-altitude ionospheric hiss. In an event study, intense hiss wave power is concentrated over a narrow frequency band with a central frequency that decreases as latitude decreases, which coincides to the variation of local proton cyclotron frequency f(CH). The wave propagates obliquely to the background magnetic field and equatorward from high latitude region. We use about similar to 6 years of observations to statistically study the dependence of ionospheric hiss wave power on location, local time, geomagnetic activity, and season. The results demonstrate that the ionospheric hiss power is stronger on the dayside than nightside, under higher geomagnetic activity conditions, in local summer than local winter. The wave power is confined near the region where the local fCH is equal to the wave frequency. A ray tracing simulation is performed to account for the dependence of wave power on frequency and latitude.
Název v anglickém jazyce
Statistical Characteristics of Ionospheric Hiss Waves
Popis výsledku anglicky
In this study, we use the observations of electromagnetic waves by Detection of Electromagnetic Emissions Transmitted from Earthquake Regions satellite to investigate propagation characteristics of low-altitude ionospheric hiss. In an event study, intense hiss wave power is concentrated over a narrow frequency band with a central frequency that decreases as latitude decreases, which coincides to the variation of local proton cyclotron frequency f(CH). The wave propagates obliquely to the background magnetic field and equatorward from high latitude region. We use about similar to 6 years of observations to statistically study the dependence of ionospheric hiss wave power on location, local time, geomagnetic activity, and season. The results demonstrate that the ionospheric hiss power is stronger on the dayside than nightside, under higher geomagnetic activity conditions, in local summer than local winter. The wave power is confined near the region where the local fCH is equal to the wave frequency. A ray tracing simulation is performed to account for the dependence of wave power on frequency and latitude.
Klasifikace
Druh
J<sub>imp</sub> - Článek v periodiku v databázi Web of Science
CEP obor
—
OECD FORD obor
10305 - Fluids and plasma physics (including surface physics)
Návaznosti výsledku
Projekt
—
Návaznosti
I - Institucionalni podpora na dlouhodoby koncepcni rozvoj vyzkumne organizace
Ostatní
Rok uplatnění
2019
Kód důvěrnosti údajů
S - Úplné a pravdivé údaje o projektu nepodléhají ochraně podle zvláštních právních předpisů
Údaje specifické pro druh výsledku
Název periodika
Geophysical Research Letters
ISSN
0094-8276
e-ISSN
—
Svazek periodika
46
Číslo periodika v rámci svazku
13
Stát vydavatele periodika
US - Spojené státy americké
Počet stran výsledku
10
Strana od-do
7147-7156
Kód UT WoS článku
000476960100010
EID výsledku v databázi Scopus
2-s2.0-85068530518