Observations of a thunderstorm density current are discussed. Because the ambient lower atmosphere was stratified, interesting interactions between the outflow current and the ambient environment resulted. The leading portion of the current was modulated by at least three gravity wavelike perturbations of horizontal spacing 12 km which initially coexisted with it. However, as the current evolved, it initiated an undular borelike disturbance which propagated ahead into the stable boundary layer, carrying cold outlfow air in large amplitude rolls. Eventually the wave family left the decelerating outflow air in its wake. This borelike disturbance resembles the Australian "morning glory' phenomenon and appears to represent an early stage in the development of a solitary wave family. The observations resemble other reported morning glories and solitary waves as well their laboratory and numerically simulated counterparts. -from Authors
CITATION STYLE
Fulton, R., Zrnic, D. S., & Doviak, R. J. (1990). Initiation of a solitary wave family in the demise of a nocturnal thunderstorm density current. Journal of the Atmospheric Sciences, 47(3), 319–337. https://doi.org/10.1175/1520-0469(1990)047<0319:IOASWF>2.0.CO;2
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