2015
DOI: 10.1002/2014ja020281
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Weak kinetic Alfvén waves turbulence during the 14 November 2012 geomagnetic storm: Van Allen Probes observations

Abstract: In the dawn sector, L ∼ 5.5 and MLT ∼4-7, from 01:30 to 06:00 UT during the 14 November 2012 geomagnetic storm, both Van Allen Probes observed an alternating sequence of locally quiet and disturbed intervals with two strikingly different power fluctuation levels and magnetic field orientations: either small (∼10 −2 nT 2 ) total power with strong GSM B x and weak B y or large (∼10 nT 2 ) total power with weak B x and strong B y and B z components. During both kinds of intervals the fluctuations occur in the vic… Show more

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Cited by 39 publications
(64 citation statements)
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“…A similar result concerning the wave mode identification has recently been reported from an analysis of a storm time broadband electromagnetic wave event by Moya et al . []. These waves are the low‐frequency electromagnetic counterpart of the electric field variations examined by Malaspina et al .…”
Section: Introductionmentioning
confidence: 88%
“…A similar result concerning the wave mode identification has recently been reported from an analysis of a storm time broadband electromagnetic wave event by Moya et al . []. These waves are the low‐frequency electromagnetic counterpart of the electric field variations examined by Malaspina et al .…”
Section: Introductionmentioning
confidence: 88%
“…The observations by Moya et al . [] show the electric power spectrum having a scaling of f −2 as observed by Radiation Belt Storm Probes (RBSP). Moya et al .…”
Section: Numerical Simulationsmentioning
confidence: 99%
“…Moya et al . [] depicted the presence of KAW in radiation belts based on their observed scalings. The KAW is low‐frequency wave in which density localization takes place due to its interaction with high‐frequency pump quasi‐electrostatic whistler.…”
Section: Numerical Simulationsmentioning
confidence: 99%
See 1 more Smart Citation
“…Recent observations from the Van Allen Probes spacecraft have revealed the prevalence at L ≳ 4 during storm times of broadband electromagnetic oscillations with some of the largest amplitude electric fields observed in the magnetosphere [Chaston et al, 2015]. These oscillations have scales transverse to the magnetic field of the order of ion gyroradii and locally have the dispersive properties of kinetic Alfvén waves [Chaston et al, 2014;Malaspina et al, 2015;Moya et al, 2015]. While kinetic Alfvén waves are narrow perpendicular to the geomagnetic field they have parallel wavelengths which in the inner magnetosphere may be of the order of the field-line length.…”
Section: Introductionmentioning
confidence: 99%