Numerical experiments are conducted using an idealized cloud-resolving model to explore the sensitivity of deep convective initiation (DCI) to the lapse rate of the active cloud-bearing layer [ACBL; the atmospheric layer above the level of free convection (LFC)]. Clouds are initiated using a new technique that involves a preexisting airmass boundary initialized such that the (unrealistic) adjustment of the model state variables to the imposed boundary is disassociated from the simulation of convection. Reference state environments used in the experiment suite have identical mixed layer values of convective inhibition, CAPE, and LFC as well as identical profiles of relative humidity and wind. Of the six simulations conducted for the experime...
A lack of routine environmental observations located near deepening cumulus congestus clouds limits ...
A method for evaluating the penetration of a stable layer by an elevated convective downdraft is dis...
The relationship between convective penetration depth and tropospheric humidity is central to recent...
Numerical experiments are conducted using an idealized cloud-resolving model to explore the sensitiv...
Using cloud-resolving simulations, this study investigates the mechanisms and sensitivities of deep-...
In this study, a 2D cloud-system-resolving model (CSRM) is used to assess the control mechanism for ...
Convective initiation (hereinafter denoted CI), defined as the development of cumulus convection int...
Convection initiation (CI) remains a forecasting challenge for meteorologists. CI frequently occurs ...
A model unifying the representation of the planetary boundary layer and dry, shallow and deep convec...
Forecasts of the timing and location of deep convection are inadequate, as are scientists’ understan...
Deep convection frequently occurs on the eastern side of upper-level troughs, or potential vorticity...
Precipitation processes in convective storms are potentially a major regulator of cloud feedback. An...
Large-eddy simulation is used to study the sensitivity of trade wind cumulus clouds to perturbations...
Cloud-resolving numerical simulations of airflow over a diurnally heated mountain ridge are conducte...
Large-eddy simulation is used to study the sensitivity of trade wind cumulus clouds to perturbations...
A lack of routine environmental observations located near deepening cumulus congestus clouds limits ...
A method for evaluating the penetration of a stable layer by an elevated convective downdraft is dis...
The relationship between convective penetration depth and tropospheric humidity is central to recent...
Numerical experiments are conducted using an idealized cloud-resolving model to explore the sensitiv...
Using cloud-resolving simulations, this study investigates the mechanisms and sensitivities of deep-...
In this study, a 2D cloud-system-resolving model (CSRM) is used to assess the control mechanism for ...
Convective initiation (hereinafter denoted CI), defined as the development of cumulus convection int...
Convection initiation (CI) remains a forecasting challenge for meteorologists. CI frequently occurs ...
A model unifying the representation of the planetary boundary layer and dry, shallow and deep convec...
Forecasts of the timing and location of deep convection are inadequate, as are scientists’ understan...
Deep convection frequently occurs on the eastern side of upper-level troughs, or potential vorticity...
Precipitation processes in convective storms are potentially a major regulator of cloud feedback. An...
Large-eddy simulation is used to study the sensitivity of trade wind cumulus clouds to perturbations...
Cloud-resolving numerical simulations of airflow over a diurnally heated mountain ridge are conducte...
Large-eddy simulation is used to study the sensitivity of trade wind cumulus clouds to perturbations...
A lack of routine environmental observations located near deepening cumulus congestus clouds limits ...
A method for evaluating the penetration of a stable layer by an elevated convective downdraft is dis...
The relationship between convective penetration depth and tropospheric humidity is central to recent...