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ممنون از توضیح خوبت مهدی جان.ولی یک سوال؟ elevated convection میتونه در cold front سیکلونها در بارشهای زمستانی هم وجود داشته باشه،یعنی همرفت از سطح زمین انجام نشه و در واقع از بالای لایهٔ inversion رخ بده.کما اینکه در فریم بعد مشهد هم cape نمودار شد و هم CIN .میشه در مورد این برام توضیح بدی؟ممنون از وقتی که میگذاری.
CAPE is effectively the positive buoyancy of an air parcel and is an indicator of atmospheric instability, which makes it very valuable in predicting severe weather. It is a form of fluid instability found in thermally stratified atmospheres in which a colder fluid overlies a warmer one. As explained below, when an air mass is unstable, the element of the air mass that is displaced upwards is accelerated by the pressure differential between the displaced air and the ambient air at the (higher) altitude to which it was displaced. This usually creates vertically developed clouds from convection, due to the rising motion, which can eventually lead to thunderstorms. It could also be created in other phenomenon, such as a cold front. Even if the air is cooler on the surface, there is still warmer air in the mid-levels, that can rise into the upper-levels. However, if there is not enough water vapor present, there is no ability for condensation, thus storms, clouds, and rain will not form.