An explicit simulation of tropical cyclones with a triply nested movable mesh primitive equation model: TCM3. Part I: Model description and control experiment

By Yuqing Wang. 2001

200 citations recorded by the source corpus.

Subfields: Atmospheric Science, Oceanography

View Paper: https://www.semanticscholar.org/paper/1b803b3c43811e7519f47bf3085a15d61a39acc3

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

In Oceanography

Citations in the corpus

An Explicit Simulation of Tropical Cyclones with a Triply Nested Movable Mesh Primitive Equation Model: TCM3. Part II: Model Refinements and Sensitivity to Cloud Microphysics Parameterization* (2002, unknown): “…a great portion of the convection can be resolved, and thus the convective parameterization is bypassed, and the explicit representation of cloud microphysics is usually included in great detail even in three-dimensional numerical models (Tripoli 1992; Liu et al. 1997, 1999; Wang 1999, 2001).”
Sensitivity of the Simulated Tropical Cyclone Inner-Core Size to the Initial Vortex Size* (2010, methodology): “This has been studied in some details in Wang (2009) and XW10 and will be discussed further in section 3b.”
Vortex Rossby Waves in a Numerically Simulated Tropical Cyclone. Part II: The Role in Tropical Cyclone Structure and Intensity Changes* (2002, methodology): “The asymmetric structure in the inner core within a radius of about 60 km is dominated by wavenumber-1 vortex Rossby waves, as already shown in Wang (2001, 2002).”
Tropical‐cyclone intensification and predictability in three dimensions (2008, methodology): “…(e.g. Zhu et al., 2001; Zhu and Smith, 2002, 2003); those using hydrostatic three-dimensional models with explicit microphysics (e.g. Wang 2001, 2002a, 2002b); and those using non-hydrostatic axisymmetric cloud models (e.g. Willoughby et al., 1984; Rotunno and Emanuel, 1987; Persing…”
Sensitivity of Tropical Cyclone Inner-Core Size and Intensity to the Radial Distribution of Surface Entropy Flux (2010, methodology): “2003), an explicit treatment of mixed-phase cloud microphysics (Wang 2001), a nonlinear fourth-order horizontal diffusion for all prognostic variables except for that related to the mass conservation equation, a simple Newtonian cooling term to mimic the radiative cooling (Rotunno and Emanuel 1987),”
Spectral (Bin) microphysics coupled with a Mesoscale Model (MM5). Part I: Model description and first results (2005, background): “Recent theoretical studies indicate that the turbulence effect is underestimated in the model, especially for drops with sizes of about 40–70 mm (e.g., Pinksy and Khain 1998; Wang 2001; Falkovich et al. 2002).”
Numerical Simulation of Hurricane Bonnie (1998). Part II: Sensitivity to Varying Cloud Microphysical Processes (2006, methodology): “Explicit hurricane simulations have now been performed using three-class ice microphysics schemes with the grid sizes of 1.5–6 km (e.g., Liu et al. 1997; Braun and Tao 2000; Wang 2001; Yau et al. 2004).”
Sensitivity of Numerical Simulation of Early Rapid Intensification of Hurricane Emily (2005) to Cloud Microphysical and Planetary Boundary Layer Parameterizations (2008, methodology): “This result agrees with the numerical simulations from Lord et al. (1984) and Wang (2002) as mentioned in the introduction.”
A Revised Approach to Ice Microphysical Processes for the Bulk Parameterization of Clouds and Precipitation (2004, background): “Wang (2001) also pointed out the importance of ice sedimentation in simulating tropical cyclone structure.”