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- W2080491822 abstract "Incoherent scatter observations at the Arecibo Observatory have shown that nighttime electron density enhancements are formed in the upper E-region and move down to merge with a stable Es-layer lying between 105–110 km. The phenomenon is strongest in winter months, and is accompanied by the presence of an underlying Es-layer near 90 km. These observations provide support for a nighttime ‘corkscrew’ mechanism which sweeps metallic ions down from higher altitudes and deposits them between 105–110 km. A statistical study of the wind shears necessary to maintain nighttime Es-layers suggests that strong layers lying below 110 km are composed primarily of long-lifetime metallic ions." @default.
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- W2080491822 date "1974-02-01" @default.
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- W2080491822 title "Downward transport of nighttime Es-layers into the lower E-region at Arecibo" @default.
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- W2080491822 doi "https://doi.org/10.1016/0021-9169(74)90042-7" @default.
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