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The main aim of this study is to establish the ability of a simple parametrization to represent adequately the microphysical processes acting in frontal rainbands. In order to do this we compare it with a more detailed parametrization in conditions typical of warm frontal and narrow cold frontal rainbands. Simulations using a 2‐dimensional diagnostic model indicate that a mixed phase parametrization is required in dynamical models of high resolution.
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G. P. Cox (1988) studied this question.
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