Convective precipitation events ( thunderstorms ) tend to produce shorter duration storm events than orographic precipitation.
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Convective precipitation falls over a certain area for a relatively short time, as convective clouds have limited horizontal extent.
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In mid-latitudes, convective precipitation is intermittent and often associated with baroclinic boundaries such as cold fronts, squall lines, and warm fronts.
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The cause may be localized convective precipitation ( intense thunderstorms ) or sudden release from an upstream impoundment created behind a dam, landslide, or glacier.
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Precipitation is distributed fairly even around the year with a small peak in summer mainly due to convective precipitation, i . e . showers and thunderstorms.
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In mid-latitudes, convective precipitation is associated with cold fronts ( often behind the front ), squall lines, and warm fronts in very moist air.
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At resolutions greater than T639, which has a grid box dimension of about, the Arakawa-Schubert convective scheme produces minimal convective precipitation, making most precipitation unrealistically stratiform in nature.
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When constructed, combined sewer systems were typically sized to carry three It is generally infeasible to treat the volume of mixed sewage and surface runoff flowing in a combined sewer during peak runoff events caused by snowmelt or convective precipitation.
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