Effects of Convective Momentum Transport on the Atmospheric Circulation in the Community Atmosphere Model, Version 3

By J. Richter, Philip J. Rasch. 2008

308 citations recorded by the source corpus.

Subfields: Atmospheric Science, Global and Planetary Change

View Paper: https://www.semanticscholar.org/paper/733bf6cd26b3c5f49ba3097837c112604d48c9f2

How researchers see this paper

The researchers whose trusted networks rank it highest, strongest advocate first. Every researcher gets a different order.

In Atmospheric Science

1. Andrew Gettelman
2. Sungsu Park
3. Hugh Morrison
4. Stephen A. Klein
5. Xiaohong Liu
6. Chris Bretherton
7. Richard B. Neale
8. J. Golaz

In Global and Planetary Change

1. Andrew Gettelman
2. Sungsu Park
3. Stephen A. Klein
4. Hugh Morrison
5. Chris Bretherton
6. Xiaohong Liu
7. Richard B. Neale
8. Peter M. Caldwell

Citations in the corpus

• The DOE E3SM Coupled Model Version 1: Description and Results at High Resolution (2019, unknown): “It features the Zhang-McFarlane (ZM; Neale et al., 2008; Richter & Rasch, 2008; Zhang & McFarlane, 1995) deep convection scheme and the Cloud-Layers Unified by Binormals (CLUBB; Golaz et al., 2002; Larson, 2017; Larson & Golaz, 2005) for macrophysics, turbulence, and shallow convection.”
• Uncertainty quantification and parameter tuning in the CAM5 Zhang‐McFarlane convection scheme and impact of improved convection on the global circulation and climate (2013, methodology): “[57] In CAM5, the deep convective process is represented by the ZM deep convection scheme originally developed by Zhang and McFarlane [1995], with several additional modifications [Gregory et al., 1997; Neale et al., 2008; Richter and Rasch, 2008; Neale et al., 2010].”
• Tropospheric Precursors of Anomalous Northern Hemisphere Stratospheric Polar Vortices (2009, background): “The tropospheric convection is upgraded compared to 3.0 to include a new treatment of the dilution of entrainment in convection (Neale et al. 2008) and of the convective momentum transport (Richter and Rasch 2008).”
• Higher-Order Turbulence Closure and Its Impact on Climate Simulations in the Community Atmosphere Model (2013, background): “CAM5 represents nearly a complete overhaul in physical parameterization options from CAM4, with the exception of the deep convection Zhang–McFarlane (ZM) scheme (Zhang and McFarlane 1995; Neale et al. 2008; Richter and Rasch 2008).”
• The Impact of Convection on ENSO: From a Delayed Oscillator to a Series of Events (2008, methodology): “Richter and Rasch (2008) show that the mean effect of CMT is to reduce the strength of the Hadley circulation through the associated Coriolis torque.”
• Climate Sensitivity of the Community Climate System Model, Version 4 (2012, background): “CAM4 now includes the effects of deep convection in the momentum equation, which has been shown to reduce many of the biases in the surface winds, tropical convection, and the Hadley circulation in CAM3 (Richter and Rasch 2008).”
• The challenge of simulating the warmth of the mid-Miocene climatic optimum in CESM1 (2013, background): “The atmospheric component is also able to resolve tropical circulation better, including improvements in the Hadley circulation and tropical convection (Richter and Rasch, 2008).”
• The Mean Climate of the Community Atmosphere Model (CAM4) in Forced SST and Fully Coupled Experiments (2013, methodology): “Subgrid-scale convective momentum transport (CMT) has been added to the existing deep convection parameterization following Richter and Rasch (2008) and the methodology of Gregory et al. (1997).”
• The University of Washington Shallow Convection and Moist Turbulence Schemes and Their Impact on Climate Simulations with the Community Atmosphere Model (2009, methodology): “5 uses 1) a finite-volume (FV) dynamical core suitable for chemical transport modeling instead of a spectral Eulerian core as the default, 2) a new land model, 3) modifications to the cumulus momentum transport (Richter and Rasch 2008) and mass-flux closure of the deep convection scheme (Neale et al”
• Toward a Physically Based Gravity Wave Source Parameterization in a General Circulation Model (2010, background): “2008) and (ii) convective momentum transport (Richter and Rasch 2008; Neale et al. 2008).”
• An Overview of the Atmospheric Component of the Energy Exascale Earth System Model (2019, methodology): “Deep convection is based upon the formulation originally described in Zhang and McFarlane (1995, hereafter ZM), with modifications by Neale Richter and Jochum (2008) and Richter and Rasch (2008).”
• The double ITCZ bias in CMIP5 models: interaction between SST, large-scale circulation and precipitation (2015, background): “One is the inclusion of the effects of deep convection in the momentum equation (Richter and Rasch 2008).”