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Journal ArticleDOI

Cloud resolving modeling of the ARM summer 1997 IOP: Model formulation, results, uncertainties, and sensitivities

TLDR
In this article, a 3D cloud resolving model (CRM) was developed to study the statistical properties of cumulus convection and applied to simulate a 28-day evolution of clouds over the Atmospheric Radiation Measurement Program (ARM) Southern Great Plains site during the summer 1997 Intensive Observation Period.
Abstract
A new three-dimensional cloud resolving model (CRM) has been developed to study the statistical properties of cumulus convection. The model was applied to simulate a 28-day evolution of clouds over the Atmospheric Radiation Measurement Program (ARM) Southern Great Plains site during the summer 1997 Intensive Observation Period. The model was forced by the large-scale advective tendencies and surface fluxes derived from the observations. The sensitivity of the results to the domain dimensionality and size, horizontal grid resolution, and parameterization of microphysics has been tested. In addition, the sensitivity to perturbed initial conditions has also been tested using a 20-member ensemble of runs. The model captures rather well the observed temporal evolution of the precipitable water and precipitation rate, although it severely underestimates the shaded cloud fraction possibly because of an inability to account for the lateral advection of clouds over the ARM site. The ensemble runs reveal t...

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Citations
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A New Moist Turbulence Parameterization in the Community Atmosphere Model

TL;DR: In this article, a new moist turbulence parameterization is presented and implemented in the Community Atmosphere Model (CAM), which is derived from Grenier and Bretherton but has been heavily modified to improve numerical stability and efficiency with the long time steps used in climate models.
Journal ArticleDOI

The University of Washington Shallow Convection and Moist Turbulence Schemes and Their Impact on Climate Simulations with the Community Atmosphere Model

TL;DR: In this paper, a new version of the University of Washington shallow cumulus parameterization is described, which includes improved treatments of lateral mixing rates into cumulus updrafts, the evaporation of precipitation and of the interaction of cumuli with the underlying subcloud layer, and a treatment of the convective inhibition-based mass-flux closure.
References
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Journal ArticleDOI

Bulk Parameterization of the Snow Field in a Cloud Model

TL;DR: In this paper, a two-dimensional, time-dependent cloud model was used to simulate a moderate intensity thunderstorm for the High Plains region, where six forms of water substance (water vapor, cloud water, cloud ice, rain, snow and hail) were simulated.
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Stratocumulus-capped mixed layers derived from a three-dimensional model

TL;DR: In this article, a three-dimensional numerical model was used to study turbulence and entrainment within mixed layers containing stratocumulus with or without parameterized cloud-top radiative cooling.
Journal ArticleDOI

A new convective adjustment scheme. Part II: Single column tests using GATE wave, BOMEX, ATEX and arctic air‐mass data sets

TL;DR: In this article, the authors proposed two deep and shallow convection schemes for tropical field experiments (GATE, BOMEX, ATEX) and an arctic air-mass transformation.
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The National Center for Atmospheric Research Community Climate Model: CCM3*

TL;DR: The latest version of the National Center for Atmospheric Research (NCAR) Community Climate Model (CCM3) is described in this article, where the changes in both physical and dynamical formulation from CCM2 to CCM3 are presented.
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