Abstract
In order to determine the values of the Dalton and the Stanton numbers, an observational study was made over a saturated barley field in the Hachirogata. flat reclaimed land located in the northern part of Japan. The mean height of the barley was about 11 cm; the roughness height for momentum was determined from the mean wind profiles as 4.24 ± 0.18 cm and the zero-plane displacement height as 0 cm. Under neutral stratification and a saturated surface, the reciprocals of the Dalton and Stanton numbers, Da-1 and St-1, were estimated. The results show that the mean value of St-1 is 12.1, and the ratio of the bulk transfer coefficient for heat to that for momentum. C H/CM, is 0.53, which are not entirely incompatible with the few results available from past observations. The mean value of Da- is 38.2. This value is larger than St-1, and fits reasonably well with the semi-empirical equation proposed by Brutsaert (1975a,b).
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References
Barton, I. J.: 1979, ‘A Parameterization of the Evaporation from Nonsaturated Surfaces’, J. Appl. Meteorol. 18, 43–47.
Brutsaert, W.: 1975a, ‘A Theory for Local Evaporation (or Heat Transfer) from Rough and Smooth Surfaces at Ground Level’, Water Resources Res. 11, 543–550.
Brutsaert, W.: 1975b, ‘The Roughness Length for Water Vapor, Sensible Heat and Other Scalars’, J. Atmos. Sci. 32, 2028–2031.
Brutsaert, W.: 1979. ‘Heat and Mass Transfer to and from Surfaces with Dense Vegetation or Similar Permeable Roughness’, Boundary-Layer Meteorol. 16, 365–388.
Brutsaert, W.: 1982, Evaporation into the Atmosphere, D. Reidel, Dordrecht, Holland, 299 pp.
Brutsaert, W. and Kustas, W. P.: 1985, ‘Evaporation and Humidity Profiles for Neutral Conditions over Rugged Hilly Terrain’, J. Climate Appl. Meteorol. 24, 915–923.
Chahuneau, F., Desjardins, R. L., Brach, E. and Verdon, R.: 1989, ‘A Micrometeorological Facility for Eddy Flux Measurements of CO2 and H2O’, J. Atmos. Oceanic Technol. 6, 193–200.
Chamberlain, A. C.: 1968, ‘Transport of Gases to and from Surfaces with Bluff and Wave-like Roughness Elements’, Quart. J. R. Meteorol. Soc. 94, 318–332.
Dyer, A. J. and Hicks, B. B.: 1970, ‘Flux-Gradient Relationships in the Constant Flux Layer’. Quart. J. Roy. Meteorol. Soc. 96, 715–721.
Garratt, J. R.: 1978, ‘Transfer Characteristics for a Heterogeneous Surface of Large Aerodynamic Roughness’, Quart. J. R. Meteorol. Soc. 104, 491–502.
Hicks, B. B., Wesely, M. L., Coulter, R. L., Hart, R. L., Durham, J. L., Speer, R. and Stedman, D. H.: 1986, ‘An Experimental Study of Sulfur and NO x Fluxes Over Grassland’, Boundary-Layer Meteorol. 34, 103–121.
Kondo, J.: 1975, ‘Air-Sea Bulk Transfer Coefficient in Diabatic Conditions’, Boundary-Layer Meteorol. 9, 91–112.
Kondo, J. and Yamazawa, H.: 1986. ‘Bulk Transfer Coefficient over a Snow Surface’, Boundary-Layer Meteorol. 34, 123–135.
Kondo, J. and Kawanaka, A.: 1986, ‘Numerical Study on the Bulk Heat Transfer Coefficient for a Variety of Vegetation Types and Densities’, Boundary-Layer Meteorol. 37, 285–296.
Koprov, B. M. and Sokolov, D. Yu.: 1973, ‘Spatial Correlation Functions of Velocity and Temperature Components in the Surface Layer of the Atmosphere’, Izv. Atmos. Oceanic. Phys. 9, 178–182.
Owen, P. R. and Thomson, W. R.: 1963, ‘Heat Transfer Across Rough Surfaces’, J. Fluid Mech. 15, 321–334.
Toya, T. and Yasuda, N.: 1988, ‘Parameterization of Evaporation from a Non-Saturated Bare Surface for Application in Numerical Prediction Models’. J. Meteorol. Soc. Japan 66, 729–739.
Yasuda, N. and Toya, T.: 1981, ‘Evaporation from Non-saturated Surface and Surface Moisture Availability’, Pap. Met. Geophys. 32, 89–98.
Yasuda, N., Kondo, J. and Sato, T.: 1986. ‘Drainage Flow Observed in a V-shaped Valley’, J. Meteorol. Soc. Japan. 64, 283–301.
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Toya, T., Mikami, M. & Yasuda, N. A determination of the Dalton and Stanton numbers over a saturated barley field. Boundary-Layer Meteorol 52, 377–395 (1990). https://doi.org/10.1007/BF00119430
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DOI: https://doi.org/10.1007/BF00119430