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  2. Convective available potential energy - Wikipedia

    en.wikipedia.org/wiki/Convective_available...

    CAPE exists within the conditionally unstable layer of the troposphere, the free convective layer (FCL), where an ascending air parcel is warmer than the ambient air. CAPE is measured in joules per kilogram of air (J/kg). Any value greater than 0 J/kg indicates instability and an increasing possibility of thunderstorms and hail.

  3. Cyclically adjusted price-to-earnings ratio - Wikipedia

    en.wikipedia.org/wiki/Cyclically_adjusted_price...

    The cyclically adjusted price-to-earnings ratio, commonly known as CAPE, [1] Shiller P/E, or P/E 10 ratio, [2] is a stock valuation measure usually applied to the US S&P 500 equity market. It is defined as price divided by the average of ten years of earnings ( moving average ), adjusted for inflation. [ 3 ]

  4. Tephigram - Wikipedia

    en.wikipedia.org/wiki/Tephigram

    Usually, temperature and dew point data from radiosondes are plotted on these diagrams to allow calculations of convective stability or convective available potential energy (CAPE). [1] Wind barbs are often plotted at the side of a tephigram to indicate the winds at different heights.

  5. Lifted index - Wikipedia

    en.wikipedia.org/wiki/Lifted_index

    The lifted index can be used in thunderstorm forecasting, however, convective available potential energy (CAPE) is considered by most as a superior measurement of instability and is preferred by many meteorologists for convection forecasting. [1]

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  7. How to Wear the Cape Trend in Real Life - AOL

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    Even better: Rather than looking like a character in a period drama when you put a cape on, the options—from preppy, to demure, to surprisingly sporty—feel modern instead of too much like a ...

  8. Convective inhibition - Wikipedia

    en.wikipedia.org/wiki/Convective_inhibition

    Conceptually, it is the opposite of CAPE. CIN hinders updrafts necessary to produce convective weather, such as thunderstorms. Although, when large amounts of CIN are reduced by heating and moistening during a convective storm, the storm will be more severe than in the case when no CIN was present. [citation needed]

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