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.
This concern is supported by Zhao et al. (2016), [19] who found that by varying
the cumulus convective precipitation parameterization in the new GFDL AM4 model they could engineer its climate sensitivity over a wide range without being able to find any clear observational constraint that favoured one version of the model over the others.
Pielke Sr., R.A., 2001: Influence of the spatial distribution of vegetation and soils on the prediction of
cumulus convective rainfall.
Not exact matches
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.
«Insights from modeling and observational evaluation of a precipitating continental
cumulus event observed during the Midlatitude Continental
Convective Clouds Experiment field campaign.»
The G - 1 flight measurements will provide information on orographic
cumulus clouds and deep
convective systems.
I have identified that you don't understand the key role for
convective cumulus clouds, and until you get a grip on that that any talk of lapse rates will make no sense.
Although the later CM5B model scores marginally less well on your KL divergence measure, it has improved representation of the
convective boundary layer and
cumulus clouds, of tropical SW CRF and of mid-level cloud coverage.
In - depth analysis reveals that the model's shallow
cumulus convection scheme tends to significantly under - produce clouds during the times when shallow
cumuli exist in the observations, while the deep
convective and stratiform cloud schemes significantly over-produce low - level clouds throughout the day.
«Insights from modeling and observational evaluation of a precipitating continental
cumulus event observed during the Midlatitude Continental
Convective Clouds Experiment field campaign.»
[Technically speaking, it is caused by increased
convective activity whereby
cumulus clouds carry latent heat from the surface of the tropical ocean into the upper troposphere.
Another issue may be that the representation of the energy balance may be incomplete merely from the spatial variance of analyzed vertical velocity, as unresolved
convective transport (
cumulus convection) may be due to updrafts not resolved by reanalysis.