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    Free Solutions of the Barotropic Vorticity Equation 

    Source: Journal of the Atmospheric Sciences:;1988:;Volume( 046 ):;issue: 012:;page 1799
    Author(s): Branstator, Grant; Opsteegh, J. D.
    Publisher: American Meteorological Society
    Abstract: Using a variational procedure, we numerically search for steady solutions to the unforced, inviscid barotropic vorticity equation on the sphere. The algorithm produces many states that have extremely small tendencies within ...
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    Primitive-Equation-Based Low-Order Models with Seasonal Cycle. Part II: Application to Complexity and Nonlinearity of Large-Scale Atmosphere Dynamics 

    Source: Journal of the Atmospheric Sciences:;2003:;Volume( 060 ):;issue: 003:;page 478
    Author(s): Achatz, Ulrich; Opsteegh, J. D.
    Publisher: American Meteorological Society
    Abstract: A recently developed class of semiempirical low-order models is utilized for the reexamination of several aspects of the complexity and nonlinearity of large-scale dynamics in a GCM. Given their low dimensionality, these ...
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    Primitive-Equation-Based Low-Order Models with Seasonal Cycle. Part I: Model Construction 

    Source: Journal of the Atmospheric Sciences:;2003:;Volume( 060 ):;issue: 003:;page 465
    Author(s): Achatz, Ulrich; Opsteegh, J. D.
    Publisher: American Meteorological Society
    Abstract: In a continuation of previous investigations on deterministic reduced atmosphere models with compact state space representation, two main modifications are introduced. First, primitive equation dynamics is used to describe ...
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    Possible Causes of Anomalies in Seasonal Mean Circulation Patterns during the 1982–83 El Niño Event 

    Source: Journal of the Atmospheric Sciences:;1985:;Volume( 042 ):;issue: 007:;page 677
    Author(s): Kok, C. J.; Opsteegh, J. D.
    Publisher: American Meteorological Society
    Abstract: For six consecutive seasons around the 1982?83 El Niño event the relation between observed anomalies in atmospheric circulation patterns and anomalies in various forcing mechanisms is diagnosed. A linear model is used in ...
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    Barotropic Instability of Planetary-Scale Flows 

    Source: Journal of the Atmospheric Sciences:;1988:;Volume( 045 ):;issue: 020:;page 2789
    Author(s): Haarsma, R. J.; Opsteegh, J. D.
    Publisher: American Meteorological Society
    Abstract: The relevance of barotropic instability for the observed low-frequency variability in the atmosphere is investigated. The stability properties of the shallow-water equations on a sphere are computed for small values of ...
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    Nonlinear Response to Anomalous Tropical Forcing 

    Source: Journal of the Atmospheric Sciences:;1988:;Volume( 046 ):;issue: 021:;page 3240
    Author(s): Haarsma, R. J.; Opsteegh, J. D.
    Publisher: American Meteorological Society
    Abstract: We have investigated the nonlinear steady-state response of a barotropic model to an estimate of the observed anomalous tropical divergence forcing for the El Niño winter of 1982/83. The 400 mb climatological flow was made ...
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    A Simulation of the January Standing Wave Pattern Including the Effects of Transient Eddies 

    Source: Journal of the Atmospheric Sciences:;1982:;Volume( 039 ):;issue: 004:;page 734
    Author(s): Opsteegh, J. D.; Vernekar, A. D.
    Publisher: American Meteorological Society
    Abstract: A steady-state, linear, two-level primitive equation model is used to simulate the January standing wave pattern as a response to mountain, diabatic and transient eddy effects. The model equations are linearized around an ...
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    Resonance in Optimal Perturbation Evolution. Part I: Two-Layer Eady Model 

    Source: Journal of the Atmospheric Sciences:;2007:;Volume( 064 ):;issue: 003:;page 673
    Author(s): de Vries, H.; Opsteegh, J. D.
    Publisher: American Meteorological Society
    Abstract: A detailed investigation has been performed of the role of the different growth mechanisms (resonance, potential vorticity unshielding, and normal-mode baroclinic instability) in the evolution of optimal perturbations ...
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    Resonance in Optimal Perturbation Evolution. Part II: Effects of a Nonzero Mean PV Gradient 

    Source: Journal of the Atmospheric Sciences:;2007:;Volume( 064 ):;issue: 003:;page 695
    Author(s): de Vries, H.; Opsteegh, J. D.
    Publisher: American Meteorological Society
    Abstract: Optimal perturbations are constructed for a two-layer ?-plane extension of the Eady model. The surface and interior dynamics is interpreted using the concept of potential vorticity building blocks (PVBs), which are zonally ...
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    Dynamics of Singular Vectors in the Semi-Infinite Eady Model: Nonzero β but Zero Mean PV Gradient 

    Source: Journal of the Atmospheric Sciences:;2006:;Volume( 063 ):;issue: 002:;page 547
    Author(s): de Vries, H.; Opsteegh, J. D.
    Publisher: American Meteorological Society
    Abstract: A nonmodal approach based on the potential vorticity (PV) perspective is used to compute the singular vector (SV) that optimizes the growth of kinetic energy at the surface for the ?-plane Eady model without an upper rigid ...
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    DSpace software copyright © 2002-2015  DuraSpace
    نرم افزار کتابخانه دیجیتال "دی اسپیس" فارسی شده توسط یابش برای کتابخانه های ایرانی | تماس با یابش
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