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Convective overshoot information


Convective 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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Convective overshoot

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Convective overshoot is a phenomenon of convection carrying material beyond an unstable region of the atmosphere into a stratified, stable region. Overshoot...

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Stratosphere

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of significant convective activity (thunderstorms) in the troposphere below may produce turbulence as a result of convective overshoot. On October 24...

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Overshooting top

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An overshooting top forms when a thunderstorm's updraft, due to momentum from rapid ascent and strength of lifting through the free convective layer...

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Pleiades

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include factors such as convective overshoot, in which a convective zone within a star penetrates an otherwise non-convective zone, resulting in higher...

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Stellar core

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throughout the convective region, and possibly in a larger region due to convective overshoot. When core fusion ceases, the core starts to collapse and it is so...

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Free convective layer

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EL gives the amount of convective available potential energy (CAPE), an estimate of the maximum energy available to convection. The depth of the FCL is...

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Falk Herwig

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Herwig, Falk (July 11, 2000). "The evolution of AGB stars with convective overshoot". University of Potsdam (Report). Cornell University Library....

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Cumulonimbus cloud

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portal Atmospheric convection Atmospheric thermodynamics Convective instability Hot tower Lifted condensation level (LCL), convective condensation level...

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Convective storm detection

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Convective storm detection is the meteorological observation, and short-term prediction, of deep moist convection (DMC). DMC describes atmospheric conditions...

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Squall line

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"Nor'wester" may be a progressive derecho. Convective storm detection Mesoscale convective complex (MCC) Mesoscale convective vortex (MCV) Mesovortex Squall Wikimedia...

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Equilibrium level

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LNB from land to sea). Atmospheric thermodynamics Convective instability Level of free convection Lifted condensation level Takahashi, Hanii; Z. Luo...

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Standard solar model

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diffusion or improvements to the treatment of convection, such as modelling turbulence, and convective overshooting. Like the Standard Model of particle physics...

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Advection

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Conservation equation Courant–Friedrichs–Lewy condition Kinematic wave Overshoot (signal) Péclet number Radiation Yin, C.; Kareem, A. (2014). "Probability...

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Tachocline

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rotating outer convective zone. This causes the region to have a very large shear as the rotation rate changes very rapidly. The convective exterior rotates...

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Lapse rate

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and the convective condensation level (CCL) when mechanical lift is absent, in which case, the parcel must be heated from below to its convective temperature...

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Convective planetary boundary layer

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The convective planetary boundary layer (CPBL), also known as the daytime planetary boundary layer (or simply convective boundary layer, CBL, when in context)...

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QUICK scheme

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dynamics QUICK, which stands for Quadratic Upstream Interpolation for Convective Kinematics, is a higher-order differencing scheme that considers a three-point...

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Glossary of tornado terms

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(CIRA) Convection Convective available potential energy (CAPE) Convective condensation level (CCL) Convective inhibition (CIN or CINh) Convective instability...

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CoRoT

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from convective bubbles crossing the convective core boundary to enter the radiative zone where they finally lose their identity (overshooting), or even...

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List of cloud types

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vertical extent. Of the multi-level genus-types, those with the greatest convective activity are often grouped separately as towering vertical. The genus...

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Maximum parcel level

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MPL (visually represented by the overshooting top, above the anvil). Dynamic processes within and between convective cells, such as updraft merging and...

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Differential rotation

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magnitude smaller than the depth of the convective envelope. A direct numerical simulation of solar convection would have to resolve this entire range...

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Accessory cloud

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examples of low level or vertical accessory clouds whilst the anvil, and overshooting top, are examples of high level accessory clouds. The condensation funnel...

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NGC 188

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Stetson, P. B. (2004). "On the Old Open Clusters M67 and NGC 188: Convective Core Overshooting, Color‐Temperature Relations, Distances, and Ages". Publications...

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Main sequence

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entirely radiative with convective zones near the surface. With decreasing stellar mass, the proportion of the star forming a convective envelope steadily increases...

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Atmospheric entry

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increases, both convective and radiative heating increase, but at different rates. At very high speeds, radiative heating will dominate the convective heat fluxes...

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Building insulation

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from inside to outside can help to reduce convective heat transfer significantly. Ensuring low convective heat transfer also requires attention to building...

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Heat burst

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surroundings. The parcel descends rapidly, warming due to compression, overshoots its equilibrium level, and reaches the surface, similar to a downburst...

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Wake low

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surroundings. The parcel descends rapidly, warming due to compression, overshoots its equilibrium level and reaches the surface, similar to a downburst...

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Supercell

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time, until a relative weakness allows a breakthrough of the cap (an overshooting top); cooler air to the right in the image may or may not form a shelf...

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