ONISHI, Ryo

TAKAHASHI, Keiko

大西, 領

高橋, 桂子

English

ONISHI, RYO

TAKAHASHI, KEIKO

Earth Simulator Research Results Repository

A Warm-Bin-Cold-Bulk Hybrid Cloud Microphysical Model

JAMSTEC Repository

2005a: A multimoment bulk microphysics parameterization. Part I: Analysis of the role of the spectral shape parameter.

2005b: A multimoment bulk microphysics parameterization. Part II: A proposed three-moment closure and scheme description.

A bulk microphysics parameterization with multiple ice precipitation categories.

A comparison of cloud resolving model simulations of trade wind cumulus with aircraft observation taken during

A detailed microphysical model within a twodimensional dynamic framework: Model description and preliminary results.

A ﬂux method for the numerical solution of the stochastic collection equation: Extension to two-dimensional particle distributions.

A new cloud physics parameterization in a large-eddy simulation model of marine stratocumulus.

A new double-moment microphysics parameterization for application in cloud and climate models. Part II: Single-column modeling of arctic clouds.

A weighted average ﬂux method for hyperbolic conservation laws.

A.,and P.Hobbs,1983:Themesoscaleand microscale structure and organization of clouds and precipitation in midlatitude cyclones. VIII: A model for the ‘‘seeder-feeder’’ process in warm-frontal rainbands.

and E.Karplus,2002:Freezingdrizzleformationinstablystratiﬁed layer clouds: The role of radiative cooling of cloud droplets,

Application of a Monte Carlo integration method to collision and coagulation growth processes of hydrometeors in a bin-type model.

Cloud and Precipitation Microphysics: Principles and Parameterizations.

Collection and coalescence efﬁciencies for accretion.

Collision, coalescence and breakup of raindrops. Part I: Experimentally established coalescence efﬁciencies and fragment size distributions in breakup.

Collision, coalescence and breakup of raindrops. Part II: Parameterization of fragment size distributions.

Collisions between small precipitation drops. Part II: Formulasfor coalescence, temporary coalescence, and satellites.

Controls on precipitation and cloudiness in simulations of trade-wind cumulus as observed during RICO.

Development of an effective double-moment cloud microphysics scheme with prognostic cloud condensation nuclei (CCN) for weather and climate models.

Development of an improved turbulent closure model for the atmospheric boundary layer.

Diagnosis of systematic differences between multiple parametrizations of warm rain microphysics 1496

Diffusional and accretional growth of water drops in a rising adiabatic parcel: Effects of the turbulent collision kernel.

Droplet growth in abinwarm-rainschemewithTwomeyCCNactivation.Atmos.

Dynamical core of an atmospheric general circulation model on a yin–yang grid.

Elements of the microphysical structure of numerically simulated nonprecipitating stratocumulus.

Evolution of rain water proﬁles resulting from pure sedimentation: Spectral vs. parameterized description.

Evolution of raindrop spectra. Part I: Solution to the stochastic collection/breakup equation using the method of moments.

Explicit forecasting of supercooled liquid water in winter storms using the MM5 mesoscale model.

Explicit forecasts of winter precipitation using an improved bulk microphysics scheme. Part II: Implementation of a new snow parameterization.

Improving a spectral bin microphysical scheme using TRMM satellite observations.

Large-eddy simulations of a drizzling, stratocumulus-topped marine boundary layer.

Mesoscale modeling of springtime arctic mixed-phase stratiform clouds using a new two-moment bulk microphysics scheme.

Modeling entrainment and ﬁnescale mixing in cumulus clouds.

Nonhydrostatic atmospheric GCM development and its computational performance. P r o c .1 1 t hW o r k s h o po nt h eU s eo fH i g h Performance Computing in Meteorology,

Numerical modeling of hailstorms and hailstone growth. Part I: Preliminary model veriﬁcation and sensitivity tests.

Numerical simulation of warm rain developmentin anaxisymmetriccloudmodel.J.Atmos.Sci.,31,

Rain production in convective clouds as simulated in an axisymmetric model with detailed microphysics. Part I: Description of the model.

Sensitivity of a cloud-resolving model to bulk and explicit bin microphysical schemes. Part II: Cloud microphysics and storm dynamics interactions.

Simulation of a supercell storm in clean and dirty atmosphere using weather research and forecast model with spectral bin microphysics.

Simulation of effects of atmospheric aerosols on deep turbulent convective clouds by using a spectral microphysics mixedphase cumulus cloud model. Part I: Model description and possible applications.

Size distribution of raindrops generated by their breakup and coalescence.

Spectral (bin) microphysics coupled with a mesoscale model (MM5). Part II: Simulation of a CaPE rain event with a squall line.

Terminal velocity and shape of cloud and precipitation drops aloft.

The effect of coalescence and condensation on rain formation in a cloud of ﬁnite vertical extent.

The evolution of drop spectra due to condensation, coalescence and breakup.

The evolution of raindrop spectra. Part II: Collisional collection/breakup and evaporation in a rain shaft.

The Kinematic Driver Model (KiD). Met Ofﬁce Tech.

The mesoscale and microscale structure and organization of clouds and precipitation in midlatitude cyclones. XII: A diagnostic modeling study of precipitation developmentinnarrowcold-frontal rainbands.J.

The nuclei of natural cloud formation. Part II: The supersaturation in natural clouds and the variation of cloud droplets concentrations.

The super-droplet method for the numerical simulation of clouds and precipitation: A particle-based and probabilistic microphysics model coupled with a non-hydrostatic model.

The supercooling of water.

The WRF single-moment 6-class microphysics scheme (WSM6).

Time-splitting methods for elastic models using forward time schemes.

Tzivion,S.,G.Feingold,and Z.Levin,1987:An efﬁcient numerical solution to the stochastic collection equation.

Understanding macrophysical outcomes of microphysical choices in simulations of shallow cumulus convection.

Yin-yang grid’’: An oversetgrid in spherical geometry.

http://www.jamstec.go.jp/jdb/ronbun/Ks00030742.pdf

A Warm-Bin-Cold-Bulk Hybrid Cloud Microphysical Model

Abstract

Similar works

Full text

Available Versions

Earth Simulator Research Results Repository

JAMSTEC Repository