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Numerical simulation of the generation of turbulence from cometary ion pick‐up
Author(s) -
Goldstein M. L.,
Roberts D. A.,
Matthaeus W. H.
Publication year - 1987
Publication title -
geophysical research letters
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 2.007
H-Index - 273
eISSN - 1944-8007
pISSN - 0094-8276
DOI - 10.1029/gl014i008p00860
Subject(s) - physics , turbulence , solar wind , computational physics , magnetohydrodynamics , comet , spectral density , magnetic field , wavenumber , spectral line , mechanics , astrophysics , optics , astronomy , statistics , mathematics , quantum mechanics
Observations of magnetic field fluctuations near comet Halley have revealed a rapid development of a Kolmogoroff‐like turbulence spectrum extending from below 10 −2 Hz to above 0.1 Hz. Spectra obtained far from the comet have a strong peak in power near the Doppler‐shifted ion‐cyclotron frequency of singly ionized water. Closer to the comet, the spectrum at higher frequencies is enhanced in power level over the background solar wind spectrum by approximately an order of magnitude. We solved the equations of incompressible MHD using a two‐dimensional 256×256 mode spectral method code to simulate this spectral evolution as an inertial range turbulent cascade. The initial conditions contained a constant magnetic field and a single coherent wave mode at a low wave number. The solar wind turbulence was modelled by a background noise spectrum having a Kolmogoroff spectral index. The coherent mode decayed into an inertial range spectrum with Kolmogoroff slope within a few eddy‐turnover times. Both the time scale and the increase in power level of the turbulence seen in the simulation are in accord with the Giotto observations.