Frequencies of wave packets of whistler-mode chorus inside its source region: a case study

• Published in: Annales geophysicae (1988) Vol. 26; no. 6; pp. 1665 - 1670
• Main Authors: Santolik, O., Macusova, E., Titova, E. E., Kozelov, B. V., Gurnett, D. A., Pickett, J. S., Trakhtengerts, V. Y., Demekhov, A. G.
• Format: Journal Article
• Language: English
• Published: Copernicus 11.06.2008; Copernicus Publications
• Subjects: Fysikk: 430; Matematikk og Naturvitenskap: 400; Mathematics and natural science: 400; Physics: 430; Rom- og plasmafysikk: 437; Space and plasma physics: 437; VDP
• ISSN: 1432-0576; 0992-7689; 1432-0576
• DOI: 10.5194/angeo-26-1665-2008

Whistler-mode chorus is a structured wave emission observed in the Earth's magnetosphere in a frequency range from a few hundreds of Hz to several kHz. We investigate wave packets of chorus using high-resolution measurements recorded by the WBD instrument on board the four Cluster spacecraft. A night-side chorus event observed during geomagnetically disturbed conditions is analyzed. We identify lower and upper frequencies for a large number of individual chorus wave packets inside the chorus source region. We investigate how these observations are related to the central position of the chorus source which has been previously estimated from the Poynting flux measurements. We observe typical frequency bandwidths of chorus of approximately 10% of the local electron cyclotron frequency. Observed time scales are around 0.1 s for the individual wave packets. Our results indicate a lower occurrence probability for lower frequencies in the vicinity of the central position of the source compared to measurements recorded closer to the outer boundaries of the source. This is in agreement with recent research based on the backward wave oscillator theory.