期刊
GEOPHYSICAL RESEARCH LETTERS
卷 32, 期 6, 页码 -出版社
AMER GEOPHYSICAL UNION
DOI: 10.1029/2004GL022321
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We employ a turbulence transport theory to explain the high-latitude radial evolution of cross helicity, or Alfvenicity, observed by the Ulysses spacecraft. Evolution is slower than at low latitudes due to weakened shear driving.
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