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- Convective_condensation_level abstract "The convective condensation level (CCL) represents the height (or pressure) where an air parcel becomes saturated when heated from below and lifted adiabatically due to buoyancy.In the atmosphere, assuming a constant water vapor mixing ratio, the dew point temperature (the temperature where therelative humidity is 100%) decreases with increasing height because the pressure of the atmosphere decreases with height. The CCL is determined by plotting the dew point (100%RH) verses altitude and locating the intersection with the actual measured temperature sounding. It marks where the cloud base begins when air is heated from below to the convective temperature, without mechanical lift. Once the CCL is determined, the surface temperature necessary to raise a mass of air to that height can be found by using the Dry Adiabatic Lapse Rate (DALR) to determine the potential temperature. In the early morning, this temperature is typically larger than the surface temperature, in the mid-afternoon, it may be the same.Compare this to the Lifting Condensation Level (LCL) where the air is lifted and cooled without first increasing the surface temperature. The LCL is less than or equal to the CCL depending on the temperature profile.Both condensation levels indicate the altitude (or pressure) where relative humidity reaches 100%. However, since the actual condensation level depends on the availability of condensation nuclei, clouds typically do not form until the relative humidity is somewhat above 100%.".
- Convective_condensation_level wikiPageExternalLink search?id=convective-condensation-level1.
- Convective_condensation_level wikiPageExternalLink 320.
- Convective_condensation_level wikiPageID "11530184".
- Convective_condensation_level wikiPageLength "2367".
- Convective_condensation_level wikiPageOutDegree "13".
- Convective_condensation_level wikiPageRevisionID "629548815".
- Convective_condensation_level wikiPageWikiLink Adiabatic.
- Convective_condensation_level wikiPageWikiLink Adiabatic_process.
- Convective_condensation_level wikiPageWikiLink Air_parcel.
- Convective_condensation_level wikiPageWikiLink Atmospheric_convection.
- Convective_condensation_level wikiPageWikiLink Atmospheric_thermodynamics.
- Convective_condensation_level wikiPageWikiLink Category:Atmospheric_thermodynamics.
- Convective_condensation_level wikiPageWikiLink Category:Severe_weather_and_convection.
- Convective_condensation_level wikiPageWikiLink Cloud_base.
- Convective_condensation_level wikiPageWikiLink Convective_temperature.
- Convective_condensation_level wikiPageWikiLink Fluid_parcel.
- Convective_condensation_level wikiPageWikiLink Lapse_rate.
- Convective_condensation_level wikiPageWikiLink Level_of_free_convection.
- Convective_condensation_level wikiPageWikiLink Lifted_condensation_level.
- Convective_condensation_level wikiPageWikiLink Lifting_condensation_level.
- Convective_condensation_level wikiPageWikiLink Saturated_fluid.
- Convective_condensation_level wikiPageWikiLink Vapor–liquid_equilibrium.
- Convective_condensation_level wikiPageWikiLinkText "Convective condensation level".
- Convective_condensation_level wikiPageWikiLinkText "convective condensation level".
- Convective_condensation_level hasPhotoCollection Convective_condensation_level.
- Convective_condensation_level wikiPageUsesTemplate Template:Climate-stub.
- Convective_condensation_level wikiPageUsesTemplate Template:Meteorological_variables.
- Convective_condensation_level wikiPageUsesTemplate Template:Reflist.
- Convective_condensation_level subject Category:Atmospheric_thermodynamics.
- Convective_condensation_level subject Category:Severe_weather_and_convection.
- Convective_condensation_level type Science.
- Convective_condensation_level type Thermodynamic.
- Convective_condensation_level comment "The convective condensation level (CCL) represents the height (or pressure) where an air parcel becomes saturated when heated from below and lifted adiabatically due to buoyancy.In the atmosphere, assuming a constant water vapor mixing ratio, the dew point temperature (the temperature where therelative humidity is 100%) decreases with increasing height because the pressure of the atmosphere decreases with height.".
- Convective_condensation_level label "Convective condensation level".
- Convective_condensation_level sameAs Niveau_de_condensation_par_convection.
- Convective_condensation_level sameAs 対流凝結高度.
- Convective_condensation_level sameAs m.02rg_0z.
- Convective_condensation_level sameAs Q3342271.
- Convective_condensation_level sameAs Q3342271.
- Convective_condensation_level wasDerivedFrom Convective_condensation_level?oldid=629548815.
- Convective_condensation_level isPrimaryTopicOf Convective_condensation_level.