scholarly journals A multiscale modeling framework model (superparameterized CAM5) with a higher‐order turbulence closure: Model description and low‐cloud simulations

2015 ◽  
Vol 7 (2) ◽  
pp. 484-509 ◽  
Author(s):  
Minghuai Wang ◽  
Vincent E. Larson ◽  
Steven Ghan ◽  
Mikhail Ovchinnikov ◽  
David P. Schanen ◽  
...  
Keyword(s):  
Multiscale Modeling ◽  
Higher Order ◽  
Turbulence Closure ◽  
Model Description ◽  
Closure Model ◽  
Modeling Framework ◽  
Turbulence Closure Model ◽  
Framework Model ◽  
Low Cloud ◽  
Multiscale Modeling Framework

scholarly journals Evaluating Low-Cloud Simulation from an Upgraded Multiscale Modeling Framework Model. Part I: Sensitivity to Spatial Resolution and Climatology

2013 ◽  
Vol 26 (16) ◽  
pp. 5717-5740 ◽  
Author(s):  
Kuan-Man Xu ◽  
Anning Cheng
Keyword(s):  
Multiscale Modeling ◽  
General Circulation ◽  
Circulation Model ◽  
Surface Energy Budget ◽  
South Pacific Convergence Zone ◽  
Convergence Zone ◽  
Vertical Resolution ◽  
Modeling Framework ◽  
Low Cloud ◽  
Multiscale Modeling Framework

Abstract The multiscale modeling framework, which replaces traditional cloud parameterizations with a 2D cloud-resolving model (CRM) in each atmospheric column, is a promising approach to climate modeling. The CRM component contains an advanced third-order turbulence closure, helping it to better simulate low-level clouds. In this study, two simulations are performed with 1.9° × 2.5° grid spacing but they differ in the vertical resolution. The number of model layers below 700 hPa increases from 6 in one simulation (IP-6L) to 12 in another (IP-12L) to better resolve the boundary layer. The low-cloud horizontal distribution and vertical structures in IP-12L are more realistic and its global mean is higher than in IP-6L and closer to that of CloudSat/Cloud–Aerosol Lidar and Infrared Pathfinder Satellite Observations (CALIPSO) observations. The spatial patterns of tropical precipitation are significantly improved; for example, a single intertropical convergence zone (ITCZ) in the Pacific, instead of double ITCZs in an earlier study that used coarser horizontal resolution and a different dynamical core in its host general circulation model (GCM), and the intensity of the South Pacific convergence zone (SPCZ), and the ITCZ in the Atlantic is more realistic. Many aspects of the global seasonal climatology agree well with observations except for excessive precipitation in the tropics. In terms of spatial correlations and patterns in the tropical/subtropical regions, most surface/vertically integrated properties show greater improvement over the earlier simulation than that with lower vertical resolution. The relationships between low-cloud amount and several large-scale properties are consistent with those observed in five low-cloud regions. There is an imbalance in the surface energy budget, which is an aspect of the model that needs to be improved in the future.

Numerical Simulation on the TIBL Structure in Shoreline Areas with a 2D Higher-Order Turbulence Closure Model

1995 ◽  
Vol 34 (2) ◽  
pp. 520-527
Author(s):  
Jiang Weimei ◽  
Wu Xiaoming ◽  
Zhou Jingnan
Keyword(s):  
Numerical Simulation ◽  
Internal Boundary Layer ◽  
Higher Order ◽  
Turbulence Closure ◽  
Internal Boundary ◽  
Initial Condition ◽  
Closure Model ◽  
Thermal Internal Boundary Layer ◽  
Turbulence Closure Model ◽  
The Mean

Abstract A 2D higher-order turbulence closure model for research on the structure of the thermal internal boundary layer (TIBL) has been developed in this paper. The mean quantities (temperature and wind), as well as their turbulent moments and their distribution under the TIBL, were computed. Results of numerical simulation show that under the initial condition of onshore flow and surface temperature on land being higher, than on water. 1) the profile of the TIBL on shore can be identified by the distributions of the mean wind and temperature, and during the integration hours there is an unstable stratified region over land that extends upward and inland gradually; 2) the shape of the profiles of the TIBL is roughly in concordance with observed profiles, but there are some differences, obviously, between the results computed by the formula of h ∼ x1/2 and the results of the numerical experiment; and 3) u′2, v′2, w′2, and u′w′, θ′w′ and their general features are well reproduced by the model. It is shown that the numerical model is feasible and effective.

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