Linked from

The 26 pages that link to Atmospheric convection, each with the reason it gives.

• Atmospheric circulationRelated: Convection drives rising branches of circulation where the atmosphere is heated.

• Latent heatRelated: Latent heat released by condensation can strengthen rising air currents.

• Water vaporRelated: Rising moist air transports vapor and releases heat as it condenses.

• CondensationRelated: Heat released by condensation can strengthen buoyant air currents.

• Intertropical Convergence ZoneRelated: Solar heating makes moist air rise where surface winds converge.

• Cloud feedbackRelated: Convection shapes the formation and altitude of many cloud types.

• Climate modelingRelated: Convection is too fine-grained for many climate grids and requires parameterization.

• Atmospheric stabilityRelated: Unstable layers allow convection to grow, while stable layers inhibit it.

• ThunderstormRelated: Buoyant air supplies the updrafts that build a thunderstorm.

• Cloud formationRelated: Convective ascent cools moist air and can produce clouds.

• Cloud genusRelated: Convection builds the vertical structure characteristic of several cloud genera.

• Lord RayleighRelated: The same competition between buoyancy and diffusion helps frame atmospheric instability.

• Rayleigh–Bénard convectionRelated: Uneven heating drives buoyant circulation in a fluid layer of air.

• Atmospheric instabilityRelated: Instability supplies the buoyant motions that initiate convection.

• Cumulus humilisRelated: Small convective currents produce the limited upward growth characteristic of this cloud.

• Altocumulus cloudRelated: Convection can build rounded altocumulus elements and produce the species castellanus.

• CloudburstRelated: Strong upward currents can build the towering clouds that produce cloudbursts.

• Edward Norton LorenzRelated: Lorenz’s simplified equations were developed to study convection.