Volume 125, Issue 6 e2020JA027793
Research Article

Conjugate Observations of Quasiperiodic Emissions by the Van Allen Probes Spacecraft and Ground‐Based Station Kannuslehto

B. Bezděková

Corresponding Author

Faculty of Mathematics and Physics, Charles University, Prague, Czech Republic

Correspondence to: B. Bezděková,

baja@etranslator.biz

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F. Němec

Faculty of Mathematics and Physics, Charles University, Prague, Czech Republic

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J. Manninen

Sodankylä Geophysical Observatory, Sodankylä, Finland

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G. B. Hospodarsky

Department of Physics and Astronomy, University of Iowa, Iowa City, IA, USA

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O. Santolík

Faculty of Mathematics and Physics, Charles University, Prague, Czech Republic

Department of Space Physics, Institute of Atmospheric Physics, The Czech Academy of Sciences, Prague, Czech Republic

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W. S. Kurth

Department of Physics and Astronomy, University of Iowa, Iowa City, IA, USA

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D. P. Hartley

Department of Physics and Astronomy, University of Iowa, Iowa City, IA, USA

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First published: 14 May 2020
Citations: 1

Abstract

Whistler mode waves observed in the Earth's inner magnetosphere at frequencies between about 0.5 and 4 kHz which exhibit a nearly periodic time modulation of the wave intensity are called quasiperiodic (QP) emissions. Conjugate measurements of QP events at several different locations can be used to estimate their spatial extent and spatiotemporal variability. Results obtained using conjugate QP measurements provided by the ground‐based station Kannuslehto (L≈5.5) and the Van Allen Probes spacecraft (L shells between about 1.1 and 6.5) between September 2012 and November 2017 are presented. Altogether, 26 simultaneously detected events were analyzed. The event modulation periods and frequency‐time structures were generally the same at all observation points. Spatial separations of the spacecraft and the ground‐based station during conjugate observations are typically within about 40° in azimuth and from about 1 to 3 in L shell. RBSP consistently observes events at lower L shells than Kannuslehto, with the event occurrence primarily inside of the plasmasphere. Ratios of Poynting fluxes observed by the spacecraft and on the ground are used to evaluate event intensity variations related to the spacecraft position. It is found that the intensity decreases considerably both at low L shells and outside of the plasmasphere. Finally, an event containing a gap in its frequency‐time structure related to a sudden change of its properties is analyzed in detail.