People ranging from Gavin Schmidt (http://www.realclimate.org/index.php/archives/2007/12/tropical-troposphere-trends/) to Richard Lindzen (who says «The dominant role of
cumulus convection in the tropics requires that temperature approximately follow what is called a moist adiabatic profile.
Not exact matches
In the baseline simulations, cumulus convection arose an hour into the exercise and generated clouds that very much resembled in appearance at least those photographed during INDOE
In the baseline simulations,
cumulus convection arose an hour into the exercise and generated clouds that very much resembled
in appearance at least those photographed during INDOE
in appearance at least those photographed during INDOEX.
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).
There may be a cap for
convection, but latent heating
in a growing
cumulus cloud (forced locally by... whatever) may eventually allow it to mushroom.
Whether the activity of
cumulus convection is determined by the variables averaged over the grid box of numerical models (100 km scale for typical GCMs, 20 km scale
in the case of «high resolution» GCM of MRI).
Slowing such overturning by reducing the horizontal differential heating could tend to allow heat to build up at lower levels until the lapse rate is more favorable to localized vertical overturning (LVO)(The two forms of overturning are not always completely distinct or separate; for example, the Hadley cell, Walker, and monsoon circulations, as well as extratropical storm track activity (developing from baroclinic instability (Rossby wave phenomena)-RRB- are driven and organized
in part by horizontal differential heating, but
in the ascending portions of these circulations,
cumulus - type
convection can occur).
Then we have to consider that the amount of water coming
in will decrease because since
convection is increasing
cumulus cloudiness is increasing.
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 da
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 da
in the observations, while the deep convective and stratiform cloud schemes significantly over-produce low - level clouds throughout the day.
«The authors demonstrate that model estimates of climate sensitivity can be strongly affected by the manner through which
cumulus cloud condensate is converted into precipitation
in a model's
convection parameterization, processes that are only crudely accounted for
in GCMs.
Thirty years later, the relevance of this study has been realized
in the development of stochastic approaches to represent
cumulus convection and its upscale energy transports, and
in the emerging efforts to resolve these multi-scale processes
in atmospheric simulations at the cloud system - resolving scale (approx. 1 km).
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).
Using a full factorial design, three schemes were changed
in the MPE: vertical diffusion, cloud microphysics, and
cumulus convection.