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    The Turbulent Structure of the Stable, Nocturnal Boundary Layer 

    Source: Journal of the Atmospheric Sciences:;1984:;Volume( 041 ):;issue: 014:;page 2202
    Author(s): Nieuwstadt, F. T. M.
    Publisher: American Meteorological Society
    Abstract: A large number of turbulence observations were made under stable conditions along a meteorological mast at Cabauw, The Netherlands. To present and organize these data we turn to the parameterized equations for the turbulent ...
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    Application of Mixed-Layer Similarity to the Observed Dispersion from a Ground-Level Source 

    Source: Journal of Applied Meteorology:;1979:;volume( 019 ):;issue: 002:;page 157
    Author(s): Nieuwstadt, F. T. M.
    Publisher: American Meteorological Society
    Abstract: The laboratory experiments of Deardorff and Willis have shown that the dispersion from a low-level source under convective conditions follows mixed-layer similarity. The convective runs of the Prairie Grass dispersion ...
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    A Rate Equation for the Inversion Height in a Nocturnal Boundary Layer 

    Source: Journal of Applied Meteorology:;1979:;volume( 019 ):;issue: 012:;page 1445
    Author(s): Nieuwstadt, F. T. M.
    Publisher: American Meteorological Society
    Abstract: The application of a self-similar profile in the integration of the temperature equation across the stable boundary layer leads to a rate equation for the inversion height. An analytic solution of the resulting equation ...
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    A Rate Equation for the Nocturnal Boundary-Layer Height 

    Source: Journal of the Atmospheric Sciences:;1981:;Volume( 038 ):;issue: 007:;page 1418
    Author(s): Nieuwstadt, F. T. M.; Tennekes, H.
    Publisher: American Meteorological Society
    Abstract: A rate equation is derived which describes the development of the boundary-layer height under stable conditions as a function of time. It takes the form of a linear relaxation equation; its solution is forced toward an ...
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    The Decay of Convective Turbulence 

    Source: Journal of the Atmospheric Sciences:;1986:;Volume( 043 ):;issue: 006:;page 532
    Author(s): Nieuwstadt, F. T. M.; Brost, R. A.
    Publisher: American Meteorological Society
    Abstract: Using simulations with a large-eddy model we have studied the decay of convective turbulence in the atmospheric boundary layer when the upward surface sensible heat flux is suddenly stopped. The decay of turbulent kinetic ...
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    The Behavior of Passive and Buoyant Plumes in a Convective Boundary Layer, as Simulated with a Large-Eddy Model 

    Source: Journal of Applied Meteorology:;1989:;volume( 028 ):;issue: 009:;page 818
    Author(s): van Haren, L.; Nieuwstadt, F. T. M.
    Publisher: American Meteorological Society
    Abstract: With a large-eddy model the large-scale flow structure of the convective boundary layer is simulated in a box of (5 ? 5 ? 2) km. The calculation is run till the turbulence has reached a quasi-steady state. At that time we ...
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    Surface layer Similarity under Nonuniform Fetch Conditions 

    Source: Journal of Climate and Applied Meteorology:;1983:;volume( 022 ):;issue: 010:;page 1800
    Author(s): Beljaars, A. C. M.; Schotanus, P.; Nieuwstadt, F. T. M.
    Publisher: American Meteorological Society
    Abstract: This paper discusses the results of a surface-layer experiment near the Cabauw meteorological mast. We measured momentum, heat and moisture fluxes at two heights, namely, 3.5 and 22.5 m. The measurements also include the ...
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    Numerical and Laboratory Study of a Horizontally Evolving Convective Boundary Layer. Part I: Transition Regimes and Development of the Mixed Layer 

    Source: Journal of the Atmospheric Sciences:;2001:;Volume( 058 ):;issue: 001:;page 70
    Author(s): Fedorovich, E.; Nieuwstadt, F. T. M.; Kaiser, R.
    Publisher: American Meteorological Society
    Abstract: Results are presented from a large eddy simulation (LES) and wind tunnel study of the turbulence regime in a horizontally evolving sheared atmospheric convective boundary layer (CBL) capped by a temperature inversion. The ...
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    Numerical and Laboratory Study of Horizontally Evolving Convective Boundary Layer. Part II: Effects of Elevated Wind Shear and Surface Roughness 

    Source: Journal of the Atmospheric Sciences:;2001:;Volume( 058 ):;issue: 006:;page 546
    Author(s): Fedorovich, E.; Nieuwstadt, F. T. M.; Kaiser, R.
    Publisher: American Meteorological Society
    Abstract: Modifications of turbulence regime in the sheared convective boundary layer (CBL) by a number of external nonbuoyant forcings are studied experimentally in a thermally stratified wind tunnel and numerically by means of ...
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    Revised Estimates for Continuous Shoreline Fumigation 

    Source: Journal of Applied Meteorology:;1979:;volume( 018 ):;issue: 002:;page 133
    Author(s): van Dop, H.; Steenkist, R.; Nieuwstadt, F. T. M.
    Publisher: American Meteorological Society
    Abstract: A model is developed to describe the dispersion of pollutants in a coastal area when stable air masses are transported inland. It is assumed that a convective mixed layer develops over land, the height of which increases ...
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