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- W2002249369 abstract "Observations from the Polar spacecraft, taken during a period of northward interplanetary magnetic field (IMF) show magnetosheath ions within the magnetosphere with velocity distributions resulting from multiple merging sites along the same field line. The observations from the TIDE instrument show two separate ion energy-time dispersions that are attributed to two widely separated (-20Re) merging sites. Estimates of the initial merging times show that they occurred nearly simultaneously (within 5 minutes.) Along with these populations, cold, ionospheric ions were observed counterstreaming along the field lines. The presence of such ions is evidence that these field lines are connected to the ionosphere on both ends. These results are consistent with the hypothesis that double merging can produce closed field lines populated by solar wind plasma. While the merging sites cannot be unambiguously located, the observations and analyses favor one site poleward of the northern cusp and a second site at low latitudes." @default.
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- W2002249369 date "2008-05-01" @default.
- W2002249369 modified "2023-09-25" @default.
- W2002249369 title "Observations of the ion signatures of double merging and the formation of newly closed field lines" @default.
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- W2002249369 doi "https://doi.org/10.1029/2008gl033910" @default.
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