Whistler-Mode Chorus Wave Duct Propagation Caused by Ultralow Frequency Wave: Event Analysis and Ray-Tracing Simulation
Identifikátory výsledku
Kód výsledku v IS VaVaI
<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F68378289%3A_____%2F25%3A00638621" target="_blank" >RIV/68378289:_____/25:00638621 - isvavai.cz</a>
Nalezeny alternativní kódy
RIV/00216208:11320/25:10510134
Výsledek na webu
<a href="https://agupubs.onlinelibrary.wiley.com/doi/10.1029/2025GL116840" target="_blank" >https://agupubs.onlinelibrary.wiley.com/doi/10.1029/2025GL116840</a>
DOI - Digital Object Identifier
<a href="http://dx.doi.org/10.1029/2025GL116840" target="_blank" >10.1029/2025GL116840</a>
Alternativní jazyky
Jazyk výsledku
angličtina
Název v původním jazyce
Whistler-Mode Chorus Wave Duct Propagation Caused by Ultralow Frequency Wave: Event Analysis and Ray-Tracing Simulation
Popis výsledku v původním jazyce
This study presents observational evidence and ray-tracing simulations demonstrating ultra-low frequency (ULF) wave-induced duct propagation of whistler-mode waves. Cluster satellite observation reveals chorus propagating quasi-parallelly at high latitudes and ULF waves. Chorus intensity enhancements correlate with refractive index increases driven by the ULF wave-induced electron density and magnetic field variations. The theoretical maximum wave normal angle for duct propagation agrees with observed angles. The ray-tracing calculations, using observation-based duct models, reproduce ducted propagation, showing the consistent relation between frequencies and wave normal angles with the observation. These findings indicate that ULF waves create ducts guiding chorus waves to high latitudes and modulate chorus intensity in the time scale of the ULF wave period. This ULF wave ducting mechanism may explain chorus wave distribution and ULF wave-modulated electron precipitation/aurora, providing new insights into wave-particle interactions in radiation belts.
Název v anglickém jazyce
Whistler-Mode Chorus Wave Duct Propagation Caused by Ultralow Frequency Wave: Event Analysis and Ray-Tracing Simulation
Popis výsledku anglicky
This study presents observational evidence and ray-tracing simulations demonstrating ultra-low frequency (ULF) wave-induced duct propagation of whistler-mode waves. Cluster satellite observation reveals chorus propagating quasi-parallelly at high latitudes and ULF waves. Chorus intensity enhancements correlate with refractive index increases driven by the ULF wave-induced electron density and magnetic field variations. The theoretical maximum wave normal angle for duct propagation agrees with observed angles. The ray-tracing calculations, using observation-based duct models, reproduce ducted propagation, showing the consistent relation between frequencies and wave normal angles with the observation. These findings indicate that ULF waves create ducts guiding chorus waves to high latitudes and modulate chorus intensity in the time scale of the ULF wave period. This ULF wave ducting mechanism may explain chorus wave distribution and ULF wave-modulated electron precipitation/aurora, providing new insights into wave-particle interactions in radiation belts.
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
<a href="/cs/project/GX25-18095X" target="_blank" >GX25-18095X: Neobvyklé módy šíření elektromagnetických vln ve Sluneční soustavě</a><br>
Návaznosti
I - Institucionalni podpora na dlouhodoby koncepcni rozvoj vyzkumne organizace
Ostatní
Rok uplatnění
2025
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
1944-8007
Svazek periodika
52
Číslo periodika v rámci svazku
17
Stát vydavatele periodika
US - Spojené státy americké
Počet stran výsledku
11
Strana od-do
e2025GL116840
Kód UT WoS článku
001559245500001
EID výsledku v databázi Scopus
2-s2.0-105015484035