Abstract
The vertical transport of horizontal momentum normal to a line of cumulonimbus observed during GATE on 14 September 1974 is against the vertical momentum gradient, contrary to the predictions of mixing-length theory. Data from repeated aircraft passes normal to the line's axis at heights from 0.15 to 5.5 km are used to document the flux and determine its source.-from Author
| Original language | English |
|---|---|
| Pages (from-to) | 1815-1834 |
| Number of pages | 20 |
| Journal | Journal of the Atmospheric Sciences |
| Volume | 40 |
| Issue number | 7 |
| DOIs | |
| State | Published - 1983 |
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