| • संवहनी संघनन तल | |
| convective: संवहनी | |
| condensation: घनीकरण दबाव द्रवण | |
| condensation level: संघनन स्तर | |
| level: सापेक्षिक स्तर | |
convective condensation level मीनिंग इन हिंदी
convective condensation level उदाहरण वाक्य
उदाहरण वाक्य
अधिक: आगे- Free convective clouds generally form at the altitude of the convective condensation level ( CCL ).
- 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.
- 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.
- 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.
- 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 ).
