摘要 : In-situ observations of a moderately strong midlatitude sporadic-E layer show a separation in altitude between distinct sublayers composed of Fe+, Mg+, and NO+. From these observations it is possible to estimate the zonal wind fie... 展开
作者 | Earle GD. Pfaff RF. Bounds SR. Kane TJ. |
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作者单位 | |
期刊名称 | 《Geophysical Research Letters》 |
总页数 | 4 |
语种/中图分类号 | 英语 / P3 |
关键词 | Intermediate |
馆藏号 | N2008EPST0000797 |