作者: C. Gurgiolo , J. L. Burch
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摘要: In their paper 'First measurements of the supersonic polar wind', Nagai et al. (1984) make point that, because ion presented in earlier publication on wind (Gurgiolo and Burch, 1982) were probably oxygen, observations not but an unspecified alternate upflow. The impression is given that oxygen considered a constituent. Allusions are also made to energy range indicating it too high measure wind. Such arguments consistent with current work being done