Convective quasi-equilibrium in midlatitude continental environment and its effect on convective parameterization

By Guang J. Zhang. 2002

195 citations recorded by the source corpus.

Subfields: Atmospheric Science, Global and Planetary Change

View Paper: https://www.semanticscholar.org/paper/9f5564ec3abe3e7b3d5040038090f69589d589a1

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Citations in the corpus

Simulations of midlatitude frontal clouds by single-column and cloud--resolving models during the Atmospheric Radiation Measurement March 2000 cloud intensive operational period (2005, unknown): “convection scheme developed by Zhang and McFarlane [1995], which is based on the same spectral rising plume concept as used in the Arakawa and Schubert [1974]”
The Cumulus Parameterization Problem: Past, Present, and Future (2004, background): “Recent examples of such studies include Brown and Bretherton (1997), Cripe and Randall (2001), and Zhang (2002).”
A mass-flux cumulus parameterization scheme for large-scale models: description and test with observations (2012, methodology): “More details can be found in Zhang (2002).”
Representing Equilibrium and Nonequilibrium Convection in Large-Scale Models (2014, unknown): “However, various studies (Emanuel 1993; Raymond 1995; Zhang 2002; Donner and Philips 2003; Raymond and Herman 2011) have pointed out that the adjustment in the boundary layer occurs on much shorter time scales than that in the free troposphere.”
The Dynamics of Idealized Convection Schemes and Their Effect on the Zonally Averaged Tropical Circulation (2007, background): “Zhang (2002, 2003), and Donner and Phillips (2003) examine the validity of the QE hypothesis using observations of convective available potential energy (CAPE).”
Intercomparison and evaluation of cumulus parametrizations under summertime midlatitude continental conditions (2002, methodology): “It is seen that deep convection schemes used in some models CCM3/SIO Scripps Institution of Oceanography version of CCM3 Kiehl et al. (1996); Hack et al. (1998); Zhang (2002) CCM3/SUNY State University of New York version of CCM3 Kiehl et al. (1996); Hack et al. (1998) are very similar.”
The dynamical core, physical parameterizations, and basic simulation characteristics of the atmospheric component AM3 of the GFDL global coupled model CM3 (2011, methodology): “The promising simulation of the tropical wave spectrum (and evidence in its favor from ﬁeld programs; e.g., Zhang 2002; Donner and Phillips 2003) suggests further research as to its impact on other aspects of ocean–atmosphere coupled simulations.”
Improved Diurnal Cycle of Precipitation in E3SM With a Revised Convective Triggering Function (2019, background): “The model errors over land are thought to be associated with unrealistically strong coupling of convection to the surface heating, which is largely controlled by solar insolation in summer (Lee et al., 2007; Xie et al., 2002; Xie & Zhang, 2000; Zhang, 2002, 2003).”