moist convection sentence in Hindi
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- The result is deep, moist convection ( DMC ), or simply, a thunderstorm.
- This type of CAPE is the maximum energy available to an ascending parcel and to moist convection.
- Deep, moist convection is essentially a thunderstorm, it is cumulus congestus clouds or cumulonimbus clouds.
- The storms are a result of moist convection in the atmosphere connected to the evaporation and condensation of water.
- We therefore conclude that moist convection is a dominant factor in converting heat flow into kinetic energy in the Jovian atmosphere,
- CAPE may also exist below the LFC, but if a layer of CIN ( subsidence ) is present, it is unavailable to deep, moist convection until CIN is exhausted.
- Moist convection had been proposed as the mechanism, said Dr . Alvin Seiff of the Ames Research Center in Mountain View, Calif ., but there was no firm evidence until now.
- In an accompanying journal article, Seiff said the new research represented " a notable advance in our knowledge of Jupiter's weather by demonstrating that moist convection occurs and transports significant amounts of energy ."
- This will remain as shallow, moist convection ( small cumulus clouds ) until breaking through the convective inhibition layer, after which DMC ensues as a parcel hits the LFC and enters the FCL, if thermal or mechanical forcing continues.
- Scientists analyzing photographs taken by the Galileo spacecraft, orbiting the largest planet in the solar system, have concluded that this moist convection of thunderstorms on Jupiter is similar to that on Earth _ only more so _ but is generated by heat from a completely different source : from deep in the planet, not from sunlight.
- A 2005 study entitled " Do Meteorologists Suppress Thunderstorms ? : Radar-Derived Statistics and the Behavior of Moist Convection " examined 28 target cities and random control points in the U . S . They were compared to their surroundings in order to determine whether these target points were weather holes or their opposite, hot spots.
- 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 ).
- If the parcel is saturated it is unstable and will rise to the LCL or CCL, and either be halted due to an inversion layer of convective inhibition, or if lifting continues, deep, moist convection ( DMC ) may ensue, as a parcel rises to the level of free convection ( LFC ), after which it enters the free convective layer ( FCL ) and usually rises to the equilibrium level ( EL ).
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