By John C. Wyngaard (auth.), R. E. Munn (eds.)
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Additional info for Boundary Layer Studies and Applications: A Special Issue of Boundary-Layer Meteorology in honor of Dr. Hans A. Panofsky (1917–1988)
Sample text
O Thus represents a variable whose sample mean (0) has been removed. (5) COHERENT STRUCTURES IN THE VERY STABLE ATMOSPHERIC BOUNDARY LAYER 47 We shall now decompose cp into two parts - a composite (cpC Z/h)Rf CV cos3 f3 ) U 2 x( f18/8)-1. (z/h)) is equivalent to the factor A in Garratt (1987). References Andre, J. C. : 1982, 'The Nocturnal Surface Inversion and Influence of Clear Air Radiative Cooling', 1. Atmos. Sci. 39, 864-878. Caughey, S. , Wyngaard, J. , and Kaimal, J. : 1979, 'Turbulence in the Evolving Stable Boundary Layer', 1. Atmos. Sci. 36, 1041-1052. Friehe, C. , LaRue, J. , Champagne, F. , Gibson, C. , and Dreyer, G. : 1975, 'Effects of Temperature and Humidity Fluctuations on the Optical Refractive Index in the Marine Boundary Layer',l. Hsu, S. : 1983, 'On the Growth of a Thermally Modified Boundary Layer by Advection of Warm Air over a Cooler Sea', 1. Geophys. Res. 88, 771-774. Johnson, H. , Lenschow, D. : 1978, 'A New Fixed Vane for Measuring Air Motion. Preprints, Fourth Symposium on Meteorological Observations and Instrumentation', Amer. Meteorol. Soc. , pp. 467-470. Mulhearn, P. : 1981, 'On the Formation of a Stably Stratified Internal Boundary Layer by Advection of Warm Air over a Cooler Sea', Boundary-Layer Meteorol21, 247-254.
