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    Zonal Momentum Balance, Potential Vorticity Dynamics, and Mass Fluxes on Near-Surface Isentropes 

    Source: Journal of the Atmospheric Sciences:;2005:;Volume( 062 ):;issue: 006:;page 1884
    Author(s): Schneider, Tapio
    Publisher: American Meteorological Society
    Abstract: While it has been recognized for some time that isentropic coordinates provide a convenient framework for theories of the global circulation of the atmosphere, the role of boundary effects in the zonal momentum balance and ...
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    The Tropopause and the Thermal Stratification in the Extratropics of a Dry Atmosphere 

    Source: Journal of the Atmospheric Sciences:;2004:;Volume( 061 ):;issue: 012:;page 1317
    Author(s): Schneider, Tapio
    Publisher: American Meteorological Society
    Abstract: A dynamical constraint on the extratropical tropopause height and thermal stratification is derived by considerations of entropy fluxes, or isentropic mass fluxes, and their different magnitudes in the troposphere and ...
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    Analysis of Incomplete Climate Data: Estimation of Mean Values and Covariance Matrices and Imputation of Missing Values 

    Source: Journal of Climate:;2001:;volume( 014 ):;issue: 005:;page 853
    Author(s): Schneider, Tapio
    Publisher: American Meteorological Society
    Abstract: Estimating the mean and the covariance matrix of an incomplete dataset and filling in missing values with imputed values is generally a nonlinear problem, which must be solved iteratively. The expectation maximization (EM) ...
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    Storm-Track Shifts under Climate Change: Toward a Mechanistic Understanding Using Baroclinic Mean Available Potential Energy 

    Source: Journal of the Atmospheric Sciences:;2016:;Volume( 074 ):;issue: 001:;page 93
    Author(s): Mbengue, Cheikh; Schneider, Tapio
    Publisher: American Meteorological Society
    Abstract: onal-mean storm-track shifts in response to perturbations in climate occur even in idealized simulations of dry atmospheres with axisymmetric forcing. Nonetheless, a generally accepted theory of the mechanisms controlling ...
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    Mechanisms of Jet Formation on the Giant Planets 

    Source: Journal of the Atmospheric Sciences:;2010:;Volume( 067 ):;issue: 011:;page 3652
    Author(s): Liu, Junjun; Schneider, Tapio
    Publisher: American Meteorological Society
    Abstract: The giant planet atmospheres exhibit alternating prograde (eastward) and retrograde (westward) jets of different speeds and widths, with an equatorial jet that is prograde on Jupiter and Saturn and retrograde on Uranus and ...
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    Formation of Jets and Equatorial Superrotation on Jupiter 

    Source: Journal of the Atmospheric Sciences:;2009:;Volume( 066 ):;issue: 003:;page 579
    Author(s): Schneider, Tapio; Liu, Junjun
    Publisher: American Meteorological Society
    Abstract: The zonal flow in Jupiter?s upper troposphere is organized into alternating retrograde and prograde jets, with a prograde (superrotating) jet at the equator. Existing models posit as the driver of the flow either differential ...
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    Convective Generation of Equatorial Superrotation in Planetary Atmospheres 

    Source: Journal of the Atmospheric Sciences:;2011:;Volume( 068 ):;issue: 011:;page 2742
    Author(s): Liu, Junjun; Schneider, Tapio
    Publisher: American Meteorological Society
    Abstract: n rapidly rotating planetary atmospheres that are heated from below, equatorial superrotation can occur through convective generation of equatorial Rossby waves. If the heating from below is sufficiently strong that ...
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    Regime Transitions of Steady and Time-Dependent Hadley Circulations: Comparison of Axisymmetric and Eddy-Permitting Simulations 

    Source: Journal of the Atmospheric Sciences:;2009:;Volume( 067 ):;issue: 005:;page 1643
    Author(s): Bordoni, Simona; Schneider, Tapio
    Publisher: American Meteorological Society
    Abstract: Steady-state and time-dependent Hadley circulations are investigated with an idealized dry GCM, in which thermal forcing is represented as relaxation of temperatures toward a radiative-equilibrium state. The latitude ?0 ...
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    The Role of Stationary Eddies in Shaping Midlatitude Storm Tracks 

    Source: Journal of the Atmospheric Sciences:;2013:;Volume( 070 ):;issue: 008:;page 2596
    Author(s): Kaspi, Yohai; Schneider, Tapio
    Publisher: American Meteorological Society
    Abstract: ransient and stationary eddies shape the extratropical climate through their transport of heat, moisture, and momentum. In the zonal mean, the transports by transient eddies dominate over those by stationary eddies, but ...
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    Storm Track Shifts under Climate Change: What Can Be Learned from Large-Scale Dry Dynamics 

    Source: Journal of Climate:;2013:;volume( 026 ):;issue: 024:;page 9923
    Author(s): Mbengue, Cheikh; Schneider, Tapio
    Publisher: American Meteorological Society
    Abstract: arth?s storm tracks are instrumental for transporting heat, momentum, and moisture and thus strongly influence the surface climate. Climate models, supported by a growing body of observational data, have demonstrated that ...
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