Here Becker et al. investigated the impact of convective organization on entrainment — a process in which warm, buoyant parcels of air become saturated with moisture;
form cumulus clouds; and mix with cooler, drier parcels of air.
Not exact matches
As the blaze burns, it generates updrafts that cool and condense,
forming fluffy
cumulus clouds.
At this point, either the
clouds can dissipate into a popcorn - like formation — which is called unaggregated convection — or other
cumulus clouds in the vicinity will pile onto them,
forming a larger
cloud cluster (aggregated convection).
When the CLIMAP data proved to be wrong, and was replaced by more reliable estimates showing a substantial tropical surface temperature drop, Lindzen had to abandon his then - current model and move on to other
forms of mischief (first the «
cumulus drying» negative water vapor feedback mechanism, since abandoned, and now the «Iris» effect
cloud feedback mechanism).
Tomás Saraceno's Trace G64 B213 and
Cumulus Filaments similarly navigate
forms inspired by nature, such as
clouds and spider webs, to imagine new spatial relationships, architectures and modes of perception.
A gathering of black plastic rulers
form a
cloud on the verge of saturation, right before the
Cumulus ruptures and it starts to rain.
As a
Cumulus cloud constantly verges on collapse, Marx's subjects border between
form and formlessness, always rich in associative and connotative density.
Cumul, as in,
cumulus, is a reference to the
forms of rounded
clouds.
Once activated, the instability shown in the Köhler curve implies that the condensational growth takes over and the newly
formed cloud droplet quickly reaches the size of few microns, as the ones we find in shallow
cumuli.
When the CLIMAP data proved to be wrong, and was replaced by more reliable estimates showing a substantial tropical surface temperature drop, Lindzen had to abandon his then - current model and move on to other
forms of mischief (first the «
cumulus drying» negative water vapor feedback mechanism, since abandoned, and now the «Iris» effect
cloud feedback mechanism).
In UP, the
cloud - resolving arrays have been upgraded to include sufficient internal resolution to explicitly generate the turbulent eddies that
form marine stratocumulus and trade
cumulus clouds.
At this point, either the
clouds can dissipate into a popcorn - like formation — which is called unaggregated convection — or other
cumulus clouds in the vicinity will pile onto them,
forming a larger
cloud cluster (aggregated convection).
Cirrus
clouds — high - altitude
clouds of ice crystals — typically
form as a byproduct of the life cycle of
cumulus towers created by rising updrafts of heated, moist air.
When there is a reduction in tropical temperature for any reason, not just volcanoes,
cumulus clouds form later, say at noon instead of their usual 11:00.
As these
cumulus convective
clouds grow taller,
cloud water droplets collide and combine into raindrops and fall out of the
cloud or continue to rise until they freeze into ice crystals and
form cirrus
clouds.