Abstract
AbstractComparisons are made between the characteristics of rainbands observed in a frontal system using a C‐band Doppler radar and dynamical mechanisms relevant on the mesoscale (∼100 km).The orientation of these rainbands, nearly aligned with the thermal wind, suggests that symmetric instability may play a role in their formation. This possible explanation of the precipitation is discussed.
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More From: Quarterly Journal of the Royal Meteorological Society
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