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    Atmospheric Energy Cycle Viewed from Wave–Mean-Flow Interaction and Lagrangian Mean Circulation 

    Source: Journal of the Atmospheric Sciences:;2001:;Volume( 058 ):;issue: 020:;page 3036
    Author(s): Iwasaki, Toshiki
    Publisher: American Meteorological Society
    Abstract: A formulation is proposed to analyze energetics of the global atmosphere. To see effects of wave?mean-flow interaction and Lagrangian mean meridional circulation from nonlinear and nongeostrophic senses, rate equations of ...
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    How Does the Vertical Profile of Baroclinicity Affect the Wave Instability? 

    Source: Journal of the Atmospheric Sciences:;2010:;Volume( 068 ):;issue: 004:;page 863
    Author(s): Iwasaki, Toshiki; Kodama, Chihiro
    Publisher: American Meteorological Society
    Abstract: he growth rate of baroclinic instability waves is generalized in terms of wave?mean flow interactions, with an emphasis on the influence of the vertical profile of baroclinicity. The wave energy is converted from the zonal ...
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    A Cascade-Type Global Energy Conversion Diagram Based on Wave–Mean Flow Interactions 

    Source: Journal of the Atmospheric Sciences:;2006:;Volume( 063 ):;issue: 012:;page 3277
    Author(s): Uno, Sachiyo; Iwasaki, Toshiki
    Publisher: American Meteorological Society
    Abstract: A cascade-type energy conversion diagram is proposed for the purpose of diagnosing the atmospheric general circulation based on wave?mean flow interactions. Mass-weighted isentropic zonal means facilitate the expression ...
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    On the Analysis of Mean Downward Velocities around the Antarctic Polar Vortex 

    Source: Journal of the Atmospheric Sciences:;2008:;Volume( 065 ):;issue: 012:;page 3989
    Author(s): Miyazaki, Kazuyuki; Iwasaki, Toshiki
    Publisher: American Meteorological Society
    Abstract: The Lagrangian characteristics of vertical motions around the Antarctic polar vortex are investigated using a general circulation model (GCM) and various analysis methods. A trace analysis that estimated the vertical ...
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    Influence of the SST Rise on Baroclinic Instability Wave Activity under an Aquaplanet Condition 

    Source: Journal of the Atmospheric Sciences:;2009:;Volume( 066 ):;issue: 008:;page 2272
    Author(s): Kodama, Chihiro; Iwasaki, Toshiki
    Publisher: American Meteorological Society
    Abstract: The influence of the sea surface temperature (SST) rise on extratropical baroclinic instability wave activity is investigated using an aquaplanet general circulation model (GCM). Two types of runs were performed: the High+3 ...
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    Impacts of Evaporation from Raindrops on Tropical Cyclones. Part II: Features of Rainbands and Asymmetric Structure 

    Source: Journal of the Atmospheric Sciences:;2010:;Volume( 067 ):;issue: 001:;page 84
    Author(s): Sawada, Masahiro; Iwasaki, Toshiki
    Publisher: American Meteorological Society
    Abstract: In this study, the impacts of evaporative cooling from raindrops on a tropical cyclone (TC) are examined using cloud-resolving simulations under an idealized condition. Part I of this study showed that evaporative cooling ...
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    Impacts of Evaporation from Raindrops on Tropical Cyclones. Part I: Evolution and Axisymmetric Structure 

    Source: Journal of the Atmospheric Sciences:;2010:;Volume( 067 ):;issue: 001:;page 71
    Author(s): Sawada, Masahiro; Iwasaki, Toshiki
    Publisher: American Meteorological Society
    Abstract: Cloud-resolving simulations of an ideal tropical cyclone (TC) on an f plane are performed to investigate the effects of evaporative cooling on the evolution and structure of a TC. Evaporative cooling has markedly different ...
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    The Gradient Genesis of Stratospheric Trace Species in the Subtropics and around the Polar Vortex 

    Source: Journal of the Atmospheric Sciences:;2008:;Volume( 065 ):;issue: 002:;page 490
    Author(s): Miyazaki, Kazuyuki; Iwasaki, Toshiki
    Publisher: American Meteorological Society
    Abstract: Mechanisms that control the formation and decay of meridional gradients in stratospheric trace species in the subtropics and around the polar vortex are investigated using a gradient genesis equation that uses mass-weighted ...
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    Diagnosis of Meridional Ozone Transport Based on Mass-Weighted Isentropic Zonal Means 

    Source: Journal of the Atmospheric Sciences:;2005:;Volume( 062 ):;issue: 004:;page 1192
    Author(s): Miyazaki, Kazuyuki; Iwasaki, Toshiki
    Publisher: American Meteorological Society
    Abstract: A transport equation based on mass-weighted isentropic zonal means applies to the diagnosis for the meridional ozone transport in the troposphere and stratosphere. The mean and eddy ozone fluxes are estimated from the ...
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    Three-Dimensional Structure of Mass-Weighted Isentropic Time-Mean Meridional Circulations 

    Source: Journal of the Atmospheric Sciences:;2018:;volume 075:;issue 006:;page 2029
    Author(s): Kanno, Yuki; Iwasaki, Toshiki
    Publisher: American Meteorological Society
    Abstract: AbstractThe present study develops a diagnostic framework for investigating the three-dimensional (3D) structure of mass-weighted isentropic time-mean (T-MIM) meridional circulations and conducts a preliminary analysis of ...
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