Linked from

The 23 pages that link to Cloud condensation nuclei, each with the reason it gives.

• NucleationRelated: These particles provide surfaces that facilitate atmospheric droplet nucleation.

• PrecipitationRelated: They provide surfaces for cloud droplets to form, an early step toward many forms of precipitation.

• AerosolRelated: Aerosols provide many of the seeds from which cloud droplets form.

• CondensationBroader topic: These particles provide surfaces for atmospheric water vapor to condense onto.

• SupersaturationRelated: They enable droplet formation when air is supersaturated with water vapor.

• Dew pointRelated: They help initiate droplets after air reaches saturation near its dew point.

• Sulfur cycleRelated: Sulfate aerosols can act as these nuclei and influence cloud brightness and lifetime.

• Aerosol-cloud interactionsBroader topic: These particles provide the initial sites for liquid cloud droplets.

• Secondary organic aerosolRelated: Secondary organic aerosol can change particle properties relevant to cloud droplet formation.

• Cumulus cloudRelated: They provide surfaces for droplets to form within a cumulus cloud.

• Cloud formationBroader topic: They provide surfaces that allow droplets to form at ordinary atmospheric supersaturations.

• Lifting condensation levelRelated: In the atmosphere, droplets usually form on these particles once saturation is reached.

• Cloud baseRelated: Droplet formation around these particles makes the saturated layer optically visible.

• RainRelated: Their abundance and properties influence how many droplets clouds contain and how they grow.

• Atmospheric aerosolRelated: Many cloud droplets begin on aerosol particles, linking aerosols to cloud properties.

• Dimethyl sulfideRelated: Dimethyl sulfide-derived sulfate can contribute particles capable of serving as cloud seeds.

• Global dimmingRelated: More nuclei can produce clouds with smaller, more numerous droplets and greater reflectivity.

• Stratocumulus cloudRelated: Their abundance influences droplet sizes and reflectivity in stratocumulus decks.

• Altostratus cloudRelated: These particles provide surfaces for liquid droplets within altostratus to form.

• PineneRelated: Pinene-derived aerosol can affect the abundance of particles available for cloud formation.

• Sea surface microlayerRelated: Microlayer-derived aerosol can affect the particles available for cloud formation.

• Cloud (meteorology)Related: They provide surfaces for droplets to form when air becomes saturated.

• Fractus cloudRelated: Droplets on these particles make the visible fragments of fractus clouds.