Abstract
Voyager 1 has been in the reservoir of energetic ions and electrons that constitutes the heliosheath since it crossed the solar wind termination shock1,2,3 on 16 December 2004 at a distance from the Sun of 94 astronomical units (1âau = 1.5âÃâ108âkm). It is now â¼22âau past the termination shock crossing4. The bulk velocity of the plasma in the radialâtransverse plane has been determined5 using measurements of the anisotropy of the convected energetic ion distribution6. Here we report that the radial component of the velocity has been decreasing almost linearly over the past three years, from â¼70âkmâsâ1 to â¼0âkmâsâ1, where it has remained for the past eight months. It now seems that Voyager 1 has entered a finite transition layer of zero-radial-velocity plasma flow, indicating that the spacecraft may be close to the heliopause, the border between the heliosheath and the interstellar plasma. The existence of a flow transition layer in the heliosheath contradicts current predictions7âgenerally assumed by conceptual modelsâof a sharp discontinuity at the heliopause.
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Acknowledgements
This work was supported at The Johns Hopkins University Applied Physics Laboratory by NASA. We are grateful to J. Aiello (for assistance with our graphical presentation) and R. McNutt (for a historical summary of heliosheath terminology).
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S.M.K. contributed most of the text; E.C.R. contributed to the text and provided theory interpretation; and R.B.D. performed the data analysis with the assistance of M.E.H.
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Krimigis, S., Roelof, E., Decker, R. et al. Zero outward flow velocity for plasma in a heliosheath transition layer. Nature 474, 359â361 (2011). https://doi.org/10.1038/nature10115
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DOI: https://doi.org/10.1038/nature10115