congestus वाक्य
उदाहरण वाक्य
मोबाइल
- Showers of moderate to heavy intensity can fall from cumulus congestus clouds.
- Cumulus congestus will mature into cumulonimbus calvus under conditions of sufficient instability.
- They form at the bases of cumulus congestus clouds over tropical and subtropical waters.
- They are very similar to cumulus congestus clouds, but at a higher level.
- However it can also occur together with cumulus congestus or cumulonimbus at a cold front.
- Any showers from stratocumulus castellanus are not usually as heavy as those from cumulus congestus.
- I wouldn't be able to tell that from a Cumulus congestus cloud though.
- Moreover, even the cumulus congestus associated with a supercell thunderstorm can be very dangerous.
- Cumulonimbus progress from overdeveloped cumulus congestus clouds and may further develop as part of a supercell.
- Stratocumulus castellanus may develop into cumulus congestus ( and even further into cumulonimbus ) under auspicious conditions.
- Deep, moist convection is essentially a thunderstorm, it is cumulus congestus clouds or cumulonimbus clouds.
- Though if they develop into cumulus mediocris cloud or the cumulus congestus cloud it may mean thunderstorms later in the day.
- Convective rain, or showery precipitation, occurs from convective clouds, e . g ., cumulonimbus or cumulus congestus.
- Convective rain, or showery precipitation, occurs from convective clouds ( e . g ., cumulonimbus or cumulus congestus ).
- In particular, in the forward area of the supercell, one can find a flanking line made of cumulus congestus or small cumulonimbus.
- If unstable altocumulus castellanus accompanies or takes the place of the main altostratus layer, cumulus congestus or cumulonimbus producing showers or thunderstorms may follow.
- Among vertically developed clouds, these may include " flammagenitus " for cumulus congestus or cumulonimbus that are formed by large scale fires or volcanic eruptions.
- The World Meteorological Organization and the American Meteorological Society do not recognize cumulus castellanus as a distinct species, but instead classify all towering cumulus clouds as Cumulus congestus.
- The World Meteorological Organization does not recognize pyrocumulus or pyrocumulonimbus as distinct cloud types, but rather classifies them respectively as cumulus ( mediocris or congestus ) and cumulonimbus.
- Pyrocumulus is not recognized by the WMO as a distinct genus or species, but is, in essence, cumulus congestus formed under special circumstances that can also cause severe turbulence.
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