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    Data Assimilation in Models with Convective Adjustment

    Source: Monthly Weather Review:;1994:;volume( 122 ):;issue: 011::page 2607
    Author:
    Miller, Robert N.
    ,
    Zaron, Edward D.
    ,
    Bennett, Andrew F.
    DOI: 10.1175/1520-0493(1994)122<2607:DAIMWC>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: Practical hydrostatic ocean models are often restricted to statically stable configurations by the use of a convective adjustment. A common way to do this is to assign an infinite boat conductivity to the water at a given level if the water column should become statically unstable. This is implemented in the form of a switch. When a statically unstable configuration is detected, it is immediately replaced with a statically stable one in which heat is conserved. In this approach, the model is no longer governed by a smooth set of equations, and usual techniques of variational data assimilation must be modified. In this note, a simple one-dimensional diffusive model is presented. Despite its simplicity, this model captures the essential behavior of the convective adjustment scheme in a widely used ocean general circulation model. Since this simple model can be derived from the more complex general circulation model, it then follows that many of the properties of the constrained system can be observed in this very simple scalar ordinary differential equation with a constraint on the solution. Techniques from the theory of optimal control are used to find solutions of a simple formulation of the variational data assimilation problem in this simple case. The optimal solution involves the solution of a nonlinear problem, even when the unconstrained dynamics are linear. In cases with discontinuous dynamics, one cannot define the adjoint of the linearized system in a straightforward manner. The very simplest variational formulation is shown to have nonunique stationary points and undesirable physical consequences. Modifications that lead to better behaved calculations and more meaningful solutions are presented. Whereas it is likely that the underlying principles from control theory are applicable to practical ocean models, the technique used to solve the simple problem may be applicable only to steady problems. Derivation of suitable techniques for initial value problems will involve a major research effort.
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      Data Assimilation in Models with Convective Adjustment

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    • Monthly Weather Review

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    contributor authorMiller, Robert N.
    contributor authorZaron, Edward D.
    contributor authorBennett, Andrew F.
    date accessioned2017-06-09T16:10:11Z
    date available2017-06-09T16:10:11Z
    date copyright1994/11/01
    date issued1994
    identifier issn0027-0644
    identifier otherams-62484.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4203381
    description abstractPractical hydrostatic ocean models are often restricted to statically stable configurations by the use of a convective adjustment. A common way to do this is to assign an infinite boat conductivity to the water at a given level if the water column should become statically unstable. This is implemented in the form of a switch. When a statically unstable configuration is detected, it is immediately replaced with a statically stable one in which heat is conserved. In this approach, the model is no longer governed by a smooth set of equations, and usual techniques of variational data assimilation must be modified. In this note, a simple one-dimensional diffusive model is presented. Despite its simplicity, this model captures the essential behavior of the convective adjustment scheme in a widely used ocean general circulation model. Since this simple model can be derived from the more complex general circulation model, it then follows that many of the properties of the constrained system can be observed in this very simple scalar ordinary differential equation with a constraint on the solution. Techniques from the theory of optimal control are used to find solutions of a simple formulation of the variational data assimilation problem in this simple case. The optimal solution involves the solution of a nonlinear problem, even when the unconstrained dynamics are linear. In cases with discontinuous dynamics, one cannot define the adjoint of the linearized system in a straightforward manner. The very simplest variational formulation is shown to have nonunique stationary points and undesirable physical consequences. Modifications that lead to better behaved calculations and more meaningful solutions are presented. Whereas it is likely that the underlying principles from control theory are applicable to practical ocean models, the technique used to solve the simple problem may be applicable only to steady problems. Derivation of suitable techniques for initial value problems will involve a major research effort.
    publisherAmerican Meteorological Society
    titleData Assimilation in Models with Convective Adjustment
    typeJournal Paper
    journal volume122
    journal issue11
    journal titleMonthly Weather Review
    identifier doi10.1175/1520-0493(1994)122<2607:DAIMWC>2.0.CO;2
    journal fristpage2607
    journal lastpage2613
    treeMonthly Weather Review:;1994:;volume( 122 ):;issue: 011
    contenttypeFulltext
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