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  2. Atmospheric instability - Wikipedia

    en.wikipedia.org/wiki/Atmospheric_instability

    Atmospheric instability is a condition where the Earth's atmosphere is considered to be unstable and as a result local weather is highly variable through distance and time. [ clarification needed ] [ 1 ] Atmospheric instability encourages vertical motion, which is directly correlated to different types of weather systems and their severity.

  3. Eady model - Wikipedia

    en.wikipedia.org/wiki/Eady_model

    Unstable modes have height, vorticity, vertical velocity, and several other atmospheric parameters with contours that tilt westward with height, though temperature contours tilt eastward with height for unstable modes. A poleward heat flux is observed in unstable modes, yielding the positive feedback necessary for cyclogenesis. Low pressure ...

  4. While you watch the eclipse, you’ll also be able to feel it

    www.aol.com/news/while-watch-eclipse-ll-able...

    Heat forces air to rise and makes the atmosphere unstable. The atmosphere then creates clouds, storms and wind to let out heat energy in an attempt to bring itself back into balance.

  5. The quick cooldown during an eclipse briefly reduces the amount of heat stored in the atmosphere. Heat forces air to rise and makes the atmosphere unstable. The atmosphere then creates clouds ...

  6. Convective instability - Wikipedia

    en.wikipedia.org/wiki/Convective_instability

    A stable atmosphere makes vertical movement difficult, and small vertical disturbances dampen out and disappear. In an unstable atmosphere, vertical air movements (such as in orographic lifting , where an air mass is displaced upwards as it is blown by wind up the rising slope of a mountain range) tend to become larger, resulting in turbulent ...

  7. Atmospheric convection - Wikipedia

    en.wikipedia.org/wiki/Atmospheric_convection

    If enough instability is present in the atmosphere, this process will continue long enough for cumulonimbus clouds to form, which supports lightning and thunder. Generally, thunderstorms require three conditions to form: moisture, an unstable airmass, and a lifting force (heat).

  8. Convective available potential energy - Wikipedia

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

    The atmosphere is warm at the surface and lower levels of the troposphere where there is mixing (the planetary boundary layer (PBL)), but becomes substantially cooler with height. The temperature profile of the atmosphere, the change in temperature, the degree that it cools with height, is the lapse rate.

  9. Ohio State athletic director Ross Bjork joined Skip Mosic on 97.1 The Fan during halftime of the Buckeyes football 45-0 win over Purdue, and while on the air, Bjork admitted "a lot of improvement ...