| • संघनन स्तर | |
| condensation: घनीकरण दबाव द्रवण | |
| level: सापेक्षिक स्तर | |
condensation level मीनिंग इन हिंदी
condensation level उदाहरण वाक्य
उदाहरण वाक्य
अधिक: आगे- 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.
