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Convective condensation level(abbrev. CCL)- The level in the atmosphere to which an air parcel, if heated from below, will rise dry adiabatically, without becoming colder than its environment just before the parcel becomes satura [..]
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Convective condensation levelThe level above the surface marking the base of a cumiliform cloud that is forming due to surface heating and rising thermals.
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Convective condensation levelIt is the height to which a parcel of air, if heated sufficiently from below, will rise adiabatically until it is just saturated (condensation starts). It approximates the base height of cumuliform clouds which are, or would be, produced by surface heating.
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Convective condensation levelThe lowest level at which condensation will occur as a result of convection due to surface heating. When condensation occurs at this level, the layer between the surface and the CCL will be thoroughly [..]
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Convective condensation level(abbrev. CCL)- The level in the atmosphere to which an air parcel, if heated from below, will rise dry adiabatically, without becoming colder than its environment just before the parcel becomes saturated. See Lifted Condensation Level (LCL).
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Convective condensation levelThe height at which a parcel of air, if heated sufficiently from below will rise adiabatically until it is saturated.
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Convective condensation levelOn a thermodynamic diagram, the point of intersection of a sounding curve (representing the vertical distribution of temperature in an atmospheric column) with the saturation mixing ratio line corresp [..]
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Convective condensation levelThe altitude at which air parcels rising with the updraft of a convection cell reaches saturation; coincides with the base of cumuliform clouds.
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Convective condensation levelThe height at which a parcel of air, if heated sufficiently from below, will rise adiabatically until it is just saturated.
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Convective condensation levelThe height at which a parcel of air, if heated sufficiently from below, will rise adiabatically until it is just saturated.
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Convective condensation level(abbrev. CCL)- The level in the atmosphere to which an air parcel, if heated from below, will rise dry adiabatically, without becoming colder than its environment just before the parcel becomes satura [..]
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Convective condensation levelThe height at which a parcel of air, if heated sufficiently from below, will rise adiabatically
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Convective condensation levelThe height at which a parcel of air, if heated sufficiently from below, will rise adiabatically until it is just saturated.
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