Frontogenesis, temperature advection and mean-sea level pressure 2/5 09zNotes:The data on this slide indicates some similarities between the environment in this case, and the environment associated with laterally translating bands. Similarities included that the banding occurred northeast of the primary surface low, south of a band of 700-500 mb frontogenesis and near the northern edge of an area of 850-700 mb warm advection. ![]() Slide 18 |