Siberia and Canada are examples of areas of frontolysis
2.
In contrary to areas of " Frontogenesis ", the areas where air masses diverge are called areas of frontolysis.
3.
The areas of dissipating squall line thunderstorms may be regions of low CAPE, low humidity, insufficient wind shear, or poor synoptic dynamics ( e . g . an upper level low filling ) leading to frontolysis.
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