The Impact of Convection on ENSO: From a Delayed Oscillator to a Series of Events

By Richard B. Neale, J. Richter, Markus Jochum. 2008

623 citations recorded by the source corpus.

Subfields: Atmospheric Science, Global and Planetary Change, Oceanography

View Paper: https://www.semanticscholar.org/paper/56b446c5eed69bcc62c1d114f47da65b5d103aa0

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Citations in the corpus

Advanced Two-Moment Bulk Microphysics for Global Models. Part II: Global Model Solutions and Aerosol–Cloud Interactions* (2015, background): “3 also has a separate moist turbulent boundary layer scheme (Bretherton and Park 2009), a shallow convective parameterization (Park and Bretherton 2009), and a deep convective scheme (Zhang and McFarlane 1995) with modifications by Neale et al. (2008).”
Atmosphere‐ocean coupled processes in the Madden‐Julian oscillation (2015, background): “Rainy and windy periods are characterized by reduced diurnal SST amplitudes, net heat flux out of the ocean, and decreasing SST.”
The Role of Atmosphere Feedbacks during ENSO in the CMIP3 Models. Part III: The Shortwave Flux Feedback (2012, background): “Other studies have demonstrated that altering the model’s convection scheme, either by adjusting individual processes (Wittenberg et al. 2003; Wu et al. 2007; Kim et al. 2008; Neale et al. 2008) or by implementing an entirely new scheme (Guilyardi et al.”
The challenge of simulating the warmth of the mid-Miocene climatic optimum in CESM1 (2013, background): “0 include the revised Zhang and McFarlane deep convection scheme in CAM4 allowing for parcel mixing (Zhang and McFarlane, 1995; Neale et al., 2008, 2010).”
The DOE E3SM Coupled Model Version 1: Description and Results at High Resolution (2019, neutral): “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.”
Global‐scale convective aggregation: Implications for the Madden‐Julian Oscillation (2015, methodology): “The convection scheme in these runs is that of Zhang and McFarlane [1995], with a dilute plume modification [Neale et al., 2008] and convective momentum transport based on Richter and Rasch [2008].”
Impact of ocean model resolution on CCSM climate simulations (2012, neutral): “5) (Neale et al. 2008; G09).”
Projected changes of extreme weather events in the eastern United States based on a high resolution climate modeling system (2012, neutral): “Compared to CAM3 (in CCSM3) and PCM, CAM4 contains significant improvement on El Niño–Southern Oscillation (ENSO) by the inclusion of sub-grid scale convective momentum transport and a dilution approximation for the calculation of convective available potential energy (CAPE) in the deep convection [”
Toward a Physically Based Gravity Wave Source Parameterization in a General Circulation Model (2010, background): “5 to include (i) a dilution approximation for the calculation of convective available potential energy (CAPE) (Neale et al. 2008) and (ii) convective momentum transport (Richter and Rasch 2008; Neale et al.”
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).”
Factors controlling the position of the Intertropical Convergence Zone on an aquaplanet (2012, background): “Various studies indicate that representations of convection in models is insufficiently sensitive to the entrainment of moisture in the lower free troposphere [Neelin et al., 2009; Derbyshire et al., 2004; Bechtold et al., 2008; Neale et al., 2008].”
The double ITCZ bias in CMIP5 models: interaction between SST, large-scale circulation and precipitation (2015, background): “The second one is a modification of the calculation of convective available potential energy (CAPE), that has been reformulated to include more realistic dilution effects through an explicit representation of entrainment (Neale et al. 2008).”
Parameterization of mixed layer eddies. III: Implementation and impact in global ocean climate simulations (2010, neutral): “5 Earth system model (Neale et al., 2008; Gent et al., 2009).”
The Low-Resolution CCSM4 (2012, background): “In CCSM4 the modification of 602 the convection scheme to account for convective plume dilution and convective 603 momentum transport is a milestone for model development, because it resulted in 604 realistic ENSO periods and amplitudes (Neale et al. 2008).”
The Evolution of Climate Sensitivity and Climate Feedbacks in the Community Atmosphere Model (2012, background): “vective closure and momentum transport described by Neale et al. (2008). The model features a complete radi-”