convective region

  • 1Convective storm detection — is the meteorological observation of deep, moist convection (DMC) and consists of detection, monitoring, and short term prediction. This term includes the minority of storms which do not produce lightning and thunder. Convective storms can… …

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  • 2Convective overshoot — is a phenomenon of convection carrying material beyond an unstable region of the atmosphere into a stratified, stable region. Overshoot is caused by the momentum of the convecting material, which carries the material beyond the unstable region.… …

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  • 3Convective available potential energy — A skew T plot showing a morning sounding with a large hydrolapse followed by an afternoon sounding showing the cooling which occurred in the mid levels resulting in an unstable atmosphere as surface parcels have now become negatively buoyant. The …

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  • 4Convective inhibition — A Skew T diagram with important features labeled Convective inhibition (CIN or CINH) is a numerical measure in meteorology that indicates the amount of energy that will prevent an air parcel from rising from the surface to the level of free… …

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  • 5Mesoscale convective system — A shelf cloud such as this one can be a sign that a squall is imminent A mesoscale convective system (MCS) is a complex of thunderstorms that becomes organized on a scale larger than the individual thunderstorms but smaller than extratropical… …

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  • 6Mesoscale convective complex — MCC moving through New England: August 2, 2006 0600 UTC A mesoscale convective complex (MCC) is a unique kind of mesoscale convective system which is defined by characteristics observed in infrared satellite imagery. They are long lived,… …

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  • 7Bounded weak echo region — Vertical cross section through a supercell showing the BWER. The bounded weak echo region, also known as a BWER or a vault, is a radar signature within a thunderstorm characterized by a local minimum in radar reflectivity at low levels which… …

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  • 82008–09 Australian region cyclone season — Season summary map First storm formed: 18 November 2008 Last storm dissipated: 28 April 2009 …

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  • 9Glossaire de la météorologie — Portail de la météorologie Glossaire de la Météorologie Sommaire : Haut A B C D E F G H I …

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  • 10Glossaire De La Météorologie — Portail de la météorologie Glossaire de la Météorologie Sommaire : Haut A B C D E F G H …

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