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    The Effects of Probe-Induced Flow Distortion on Atmospheric Turbulence Measurements: Extension to Scalars 

    Source: Journal of the Atmospheric Sciences:;1988:;Volume( 045 ):;issue: 022:;page 3400
    Author(s): Wyngaard, J. C.
    Publisher: American Meteorological Society
    Abstract: I prove that in a steady velocity field the frequency spectrum of a conservative scalar is unaffected by flow distortion. This is a good approximation in turbulent flow if (qa1/3;/U1l1/3;) ? 1, where q and l are velocity ...
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    Reply 

    Source: Journal of the Atmospheric Sciences:;1985:;Volume( 042 ):;issue: 010:;page 1086
    Author(s): Wyngaard, J. C.
    Publisher: American Meteorological Society
    Abstract: No abstract availble.
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    A Physical Mechanism for the Asymmetry in Top-Down and Bottom-Up Diffusion 

    Source: Journal of the Atmospheric Sciences:;1987:;Volume( 044 ):;issue: 007:;page 1083
    Author(s): Wyngaard, J. C.
    Publisher: American Meteorological Society
    Abstract: Recent large-eddy simulations of the vertical diffusion of a passive, conservative scalar through the convective boundary layer (CBL) show strikingly different eddy diffusivity profiles in the ?top-down? and ?bottom-up? ...
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    The Effects of Probe-Induced Flow Distortion on Atmospheric Turbulence Measurements 

    Source: Journal of Applied Meteorology:;1981:;volume( 020 ):;issue: 007:;page 784
    Author(s): Wyngaard, J. C.
    Publisher: American Meteorological Society
    Abstract: We present a theory for probe-induced flow distortion which is applicable in the atmosphere at heights greater than about 10 times the obstacle size. We use the theory to calculate the behavior of Reynolds shear stress and ...
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    Structure–Function Parameters in the Convective Boundary Layer from Large-Eddy Simulation 

    Source: Journal of the Atmospheric Sciences:;1995:;Volume( 052 ):;issue: 021:;page 3641
    Author(s): Peltier, L. J.; Wyngaard, J. C.
    Publisher: American Meteorological Society
    Abstract: The conventional theory of the scattering of transmitted acoustic, microwave, and optical radiation by turbulence uses the refractive index structure-function parameter CN2. The authors calculate the vertical profiles of ...
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    Behavior of the Refractive Index Structure Parameter in the Entraining Convective Boundary Layer 

    Source: Journal of the Atmospheric Sciences:;1980:;Volume( 037 ):;issue: 007:;page 1573
    Author(s): Wyngaard, J. C.; LeMone, M. A.
    Publisher: American Meteorological Society
    Abstract: The refractive index structure parameter CN2 has contributions from the temperature and humidity structure parameters Cr2 and CQ2 and from the joint structure parameter CTQ. We briefly review the behavior of these structure ...
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    A Sharp Cutoff Spectral Differentiator 

    Source: Journal of Applied Meteorology:;1967:;volume( 006 ):;issue: 005:;page 952
    Author(s): Wyngaard, J. C.; Lumley, J. L.
    Publisher: American Meteorological Society
    Abstract: Design data and experimental results are presented for an eight-pole optimally flat filter which makes available the first seven derivatives of the filtered input signal.
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    Effect of Baroclinicity on Wind Profiles and the Geostrophic Drag Law for the Convective Planetary Boundary Layer 

    Source: Journal of the Atmospheric Sciences:;1975:;Volume( 032 ):;issue: 004:;page 767
    Author(s): Arya, S. P. S.; Wyngaard, J. C.
    Publisher: American Meteorological Society
    Abstract: By using a simple physical model of the baroclinic convective planetary boundary layer, the similarity functions of the geostrophic drag law are expressed as sums of a barotropic part, dependent only on the stability and ...
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    Taylor's Hypothesis and High–Frequency Turbulence Spectra 

    Source: Journal of the Atmospheric Sciences:;1977:;Volume( 034 ):;issue: 006:;page 922
    Author(s): Wyngaard, J. C.; Clifford, S. F.
    Publisher: American Meteorological Society
    Abstract: Lumley's model for interpreting frequency spectra of streamwise velocity in high-turbulence level flows assumes 1) that the convection velocity fluctuations and the convected finestructure are statistically independent, ...
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    A Model Study of the Stably Stratified Planetary Boundary Layer 

    Source: Journal of the Atmospheric Sciences:;1978:;Volume( 035 ):;issue: 008:;page 1427
    Author(s): Brost, R. A.; Wyngaard, J. C.
    Publisher: American Meteorological Society
    Abstract: A second-order turbulence model is used to study the stable boundary layer (SBL). Over a horizontal surface, a constant surface cooling rate drives the SBL to a steady state within a few hours. Parameterizations are developed ...
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