condensation level वाक्य
उदाहरण वाक्य
मोबाइल
- Free convective clouds generally form at the altitude of the convective condensation level ( CCL ).
- Both condensation levels indicate the altitude ( or pressure ) where relative humidity reaches 100 %.
- Alternatively, the cloud base can be estimated from surface measurements of air temperature and humidity by calculating the lifted condensation level.
- Compare this to the Lifting Condensation Level ( LCL ) where the air is lifted and cooled without first increasing the surface temperature.
- In the lower troposphere, more moisture ( small dew point depression ) results in lower cloud bases and lifted condensation levels ( LCL ).
- An absence of sufficient condensation particles at and above the condensation level causes the rising air to become supersaturated and the formation of cloud tends to be inhibited.
- The droplets would normally evaporate below the condensation level, but strong updrafts buffer the falling droplets, and can keep them aloft much longer than they would otherwise.
- 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 %.
- With the help of these lines, parameters such as cloud condensation level, level of free convection, onset of cloud formation . etc . can be derived from the soundings.
- For non-convective cloud, the altitude at which condensation begins to happen is called the lifted condensation level ( LCL ), which roughly determines the height of the cloud base.
- In the American West, the base of cumulus clouds can reach, since the combination of a low dew point ( ) and high temperature ( up to ) will yield a very high convective condensation level.
- The usual way of finding the LFC is to lift a parcel from a lower level along the dry adiabatic lapse rate until it crosses the mixing ratio line of the parcel : this is the lifted condensation level ( LCL ).
- This altitude is known as the lifting condensation level ( LCL ) when mechanical lift is present and the convective condensation level ( CCL ) when mechanical lift is absent, in which case, the parcel must be heated from below to its convective temperature.
- This altitude is known as the lifting condensation level ( LCL ) when mechanical lift is present and the convective condensation level ( CCL ) when mechanical lift is absent, in which case, the parcel must be heated from below to its convective temperature.
- If the environmental lapse rate is larger than the dry adiabatic lapse rate, it has a superadiabatic lapse rate, the air is absolutely unstable a parcel of air will gain buoyancy as it rises both below and above the lifting condensation level or convective condensation level.
- If the environmental lapse rate is larger than the dry adiabatic lapse rate, it has a superadiabatic lapse rate, the air is absolutely unstable a parcel of air will gain buoyancy as it rises both below and above the lifting condensation level or convective condensation level.
- When there is mechanical lift to saturation, cloud base begins at the lifted condensation level ( LCL ); absent forcing, cloud base begins at the convective condensation level ( CCL ) where heating from below causes spontaneous buoyant lifting to the point of condensation when the convective temperature is reached.
- When there is mechanical lift to saturation, cloud base begins at the lifted condensation level ( LCL ); absent forcing, cloud base begins at the convective condensation level ( CCL ) where heating from below causes spontaneous buoyant lifting to the point of condensation when the convective temperature is reached.
- The second favorable feature on the plot is the steep vertical temperature gradient in the lower atmosphere up to the Lifted condensation level ( LCL )-from 26.4 C at the surface ( 989 mb ) to about " 5 C at the LCL, which is about 600 mb.
- This work comes from increasing instability in the low levels by raising the temperature or dew point, or by mechanical lift . Without the aid of mechanical forcing, a parcel must reach its convective temperature ( T c ) before moist convection ( cloud ) begins near the convective condensation level ( CCL }, whereas with dynamic lift, cloud base begins near the lifted condensation level ( LCL ).
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