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    A Top-Down and Bottom-Up Diffusion Model of CT2 and CQ2 in the Entraining Convective Boundary Layer 

    Source: Journal of the Atmospheric Sciences:;1987:;Volume( 044 ):;issue: 006:;page 1009
    Author(s): Fairall, C. W.
    Publisher: American Meteorological Society
    Abstract: A model of scalar structure function parameters in the entraining, convective boundary layer is developed based on a top-down and bottom-up diffusion approach. The behavior of the structure function parameters is obtained ...
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    Wind Shear Enhancement of Entrainment and Refractive Index Structure Parameter at the Top of a Turbulent Mixed Layer 

    Source: Journal of the Atmospheric Sciences:;1984:;Volume( 041 ):;issue: 024:;page 3472
    Author(s): Fairall, C. W.
    Publisher: American Meteorological Society
    Abstract: A model for inversion layer turbulence properties of a cloud-free entraining mixed-layer with wind shear at the top is developed. Using the approach of Wyngaard and LeMone (1980), expressions for the average values of ? ...
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    The Humidity and Temperature Sensitivity of Clear-Air Radars in the Convective Boundary Layer 

    Source: Journal of Applied Meteorology:;1991:;volume( 030 ):;issue: 008:;page 1064
    Author(s): Fairall, C. W.
    Publisher: American Meteorological Society
    Abstract: A top-down/bottom-up diffusion Model is used to evaluate the relative contributions of humidity temperature, and their cross correlation to the radar refractive index structure function paramer Cn2 in the cloud-free, ...
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    Upward Momentum Transfer in the Marine Boundary Layer 

    Source: Journal of Physical Oceanography:;2001:;Volume( 031 ):;issue: 007:;page 1698
    Author(s): Grachev, A. A.; Fairall, C. W.
    Publisher: American Meteorological Society
    Abstract: This paper focuses on the study of momentum flux between ocean and atmosphere in light winds and is based on the data collected during several field campaigns, the Atlantic Stratocumulus Transition Experiment, the Tropical ...
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    Dependence of the Monin–Obukhov Stability Parameter on the Bulk Richardson Number over the Ocean 

    Source: Journal of Applied Meteorology:;1997:;volume( 036 ):;issue: 004:;page 406
    Author(s): Grachev, A. A.; Fairall, C. W.
    Publisher: American Meteorological Society
    Abstract: Recent measurements made onboard the R/P FLIP in the San Clemente Ocean Probing Experiment in September 1993 and onboard the R/V Moana Wave during Tropical Ocean Global Atmosphere Coupled Ocean?Atmosphere Response Experiment ...
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    Similarity Relationships in the Marine Atmospheric Surface Layer for Terms in the TKE and Scalar Variance Budgets 

    Source: Journal of the Atmospheric Sciences:;1998:;Volume( 055 ):;issue: 013:;page 2311
    Author(s): Edson, J. B.; Fairall, C. W.
    Publisher: American Meteorological Society
    Abstract: Measurements of the momentum, heat, moisture, energy, and scalar variance fluxes are combined with dissipation estimates to investigate the behavior of marine surface layer turbulence. These measurements span a wide range ...
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    Modeling Wind Speed Dependence of Marine Aerosol Distribution by a Gamma Function 

    Source: Journal of Applied Meteorology:;1982:;volume( 021 ):;issue: 005:;page 666
    Author(s): Goroch, Andreas K.; Fairall, C. W.; Davidson, K. L.
    Publisher: American Meteorological Society
    Abstract: Marine aerosol size distributions are fit to a gamma function using the technique of maximum likelihood. Aerosol measurements are separated into marine and continental components. The marine component is fit to the gamma ...
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    Mixed and Dynamic Response of Hot Wires and Cold Wires and Measurements of Turbulence Statistics 

    Source: Journal of Atmospheric and Oceanic Technology:;1986:;volume( 003 ):;issue: 002:;page 236
    Author(s): Larsen, S. E.; Hojstrup, J.; Fairall, C. W.
    Publisher: American Meteorological Society
    Abstract: Hot wires respond to temperature as well as to velocity, whereas cold wires respond to velocity as well as to temperature. The static and dynamic response characteristics are summarized and it is shown that the frequency ...
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    Ship Observations of the Tropical Pacific Ocean along the Coast of South America 

    Source: Journal of Climate:;2009:;volume( 022 ):;issue: 002:;page 458
    Author(s): de Szoeke, S. P.; Fairall, C. W.; Pezoa, Sergio
    Publisher: American Meteorological Society
    Abstract: In October 2007 the NOAA ship Ronald H. Brown sailed southward within 300 km of the coast of Ecuador and Peru, sampling surface meteorology, air?sea turbulent and radiative fluxes, cloud properties, and upper-air soundings ...
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    Measurement of Stratus Cloud and Drizzle Parameters in ASTEX with a Kα-Band Doppler Radar and a Microwave Radiometer 

    Source: Journal of the Atmospheric Sciences:;1995:;Volume( 052 ):;issue: 016:;page 2788
    Author(s): Frisch, A. S.; Fairall, C. W.; Snider, J. B.
    Publisher: American Meteorological Society
    Abstract: Data are used from a Kα-band radar and microwave radiometer along with a droplet model to determine the droplet parameters of drizzle and clouds. Drizzle droplet parameters are determined from the zeroth, first, and second ...
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