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
CITATION STYLE
Lemone, M. A. (1983). Momentum transport by a line of cumulonimbus. Journal of the Atmospheric Sciences, 40(7), 1815–1834. https://doi.org/10.1175/1520-0469(1983)040<1815:MTBALO>2.0.CO;2
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