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  2. Condensation cloud - Wikipedia

    en.wikipedia.org/wiki/Condensation_cloud

    A transient condensation cloud, also called a Wilson cloud, is observable surrounding large explosions in humid air. When a nuclear weapon or high explosive is detonated in sufficiently humid air, the "negative phase" of the shock wave causes a rarefaction of the air surrounding the explosion but not of the air contained within it.

  3. Twomey effect - Wikipedia

    en.wikipedia.org/wiki/Twomey_effect

    The Twomey effect describes how additional cloud condensation nuclei (CCN), possibly from anthropogenic pollution, may increase the amount of solar radiation reflected by clouds. This is an indirect effect (or radiative forcing ) by such particles, as distinguished from direct effects (forcing) due to enhanced scattering or absorbing radiation ...

  4. Funnel cloud - Wikipedia

    en.wikipedia.org/wiki/Funnel_cloud

    The term condensation funnel may refer to either a tornadic cloud or a funnel cloud aloft, but the term funnel cloud exclusively refers to a rotating condensation funnel not reaching the surface. If strong cyclonic winds are occurring at the surface and are connected to a cloud base, regardless of condensation, then the feature is a tornado. [3]

  5. Cloud physics - Wikipedia

    en.wikipedia.org/wiki/Cloud_physics

    the cloud IR emissivity, with values between 0 and 1, with a global average around 0.7; the effective cloud amount, the cloud amount weighted by the cloud IR emissivity, with a global average of 0.5; the cloud (visible) optical depth varies within a range of 4 and 10. the cloud water path for the liquid and solid (ice) phases of the cloud particles

  6. Cloud condensation nuclei - Wikipedia

    en.wikipedia.org/wiki/Cloud_condensation_nuclei

    A typical raindrop is about 2 mm in diameter, a typical cloud droplet is on the order of 0.02 mm, and a typical cloud condensation nucleus is on the order of 0.0001 mm or 0.1 μm or greater in diameter. [1] The number of cloud condensation nuclei in the air can be measured at ranges between around 100 to 1000 per cm 3. [1]

  7. Vapor cone - Wikipedia

    en.wikipedia.org/wiki/Vapor_cone

    A vapor cone (also known as a Mach diamond, [1] shock collar, or shock egg) is a visible cloud of condensed water that can sometimes form around an object moving at high speed through moist air, such as an aircraft flying at transonic speeds. When the localized air pressure around the object drops, so does the air temperature.

  8. Cloud point - Wikipedia

    en.wikipedia.org/wiki/Cloud_point

    The cloud point is analogous to the 'dew point' at which a gas-liquid phase transition called condensation occurs in water vapour (humid air) to form liquid water (dew or clouds). When the temperature is below 0 °C, the dew point is called the frost point, as water vapour undergoes gas-solid phase transition called deposition , solidification ...

  9. Condensation (disambiguation) - Wikipedia

    en.wikipedia.org/wiki/Condensation_(disambiguation)

    Condensation is the change of the state of matter from the gas phase into the liquid phase. Condensation may also refer to: DNA condensation, the process of compacting DNA molecules; Cloud condensation nuclei, airborne particles required for cloud formation; Condensation (aerosol dynamics), a phase transition from gas to liquid