Abstract
The dynamical and microphysical structures of trains of wavelike rainbands in an occlusion are described. The rainbands were located in a region of potential instability behind the cold front aloft. They were 3-5km wide, about 80km long, spaced 5-10km apart, and arranged nearly parallel to the winds at their upper levels.-from Authors
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CITATION STYLE
Wang, P. Y., & Hobbs, P. V. (1983). The mesoscale and microscale structure and organization of clouds and precipitation in midlatitude cyclones. X: wavelike rainbands in an occlusion. Journal of the Atmospheric Sciences, 40(8), 1950–1964. https://doi.org/10.1175/1520-0469(1983)040<1950:TMAMSA>2.0.CO;2
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