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Evidence for the trough wind (1972)

Brinton, H.

In: CASI

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Publication Date: 2005-11-30

Description: The existence of an upward flow of ionization along trough-field lines located at approximately 65 deg magnetic latitude is discussed. A flux model that fits the observed behavior of h(+0) and 0(+) was developed based on the existence of a trough wind. The measurements indicate a different behavior in the altitude distribution of ionized hydrogen in the plasmasphere as compared to the trough region. This difference is explained by the trough wind.

Keywords: METEOROLOGY

Type: Significant Accomplishments in Sci., 1970; p 52-57

Format: text

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