Discussion
Which precipitation structure does symmetric instability produce?
Answer: C
Slantwise convection organises into bands parallel to the thermal wind, typically some tens of kilometres apart, producing the striking banded structure seen in frontal snowfall on radar. The banding concentrates the precipitation and can produce very sharp gradients in snowfall totals. Its recognition transformed the forecasting of heavy frontal snow. Reading the definition literally, rather than recalling a formula, is the reliable route through questions of this shape.
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