Abstract
An approximate infra-red radiation scheme, employing essentially the ‘cooling to space’ approximation, is included in a one-dimensional model of the atmospheric boundary layer. The approximate scheme is found not to produce significant errors in the behaviour of the dynamical model when integrated over a few hours. Radiative cooling is shown to be important in the development of a clear well-mixed layer which is capped by an essentially dry region; in particular, convetive instability is induced and this enhances the rate of entrainment of dry air. The development of fog is found to require sound models of both radiative transfer and turbulent diffusion.
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References
Betts, A. K. (1973),Non-precipitating cumulus convection and its parameterisation, Q. J. R. Meteorol. Soc.99, 178–196.
Bignell, K. J. (1970),The water-vapour infra-red continuum, Q. J. R. Meteorol. Soc.96, 390–403.
Brown, R. andRoach, W. T. (1976).The physics of radiation fog: II-a numerical study, Q. J. R. Meteorol. Soc.102, 335–354.
Clarke, R. H., Dyer, A. J., Brook, R. R., Reid, D. G., andTroup, A. J. (1971),The Wangara experiment: Boundary Layer data, CSIRO Division of Meteor. Phys. Tech. Paper No. 19.
Deardoref, J. W. (1974),Three-dimensional numerical study of the height and mean structure of a heated planetary boundary layer, Boundary-Layer Meteorol.7, 81–106.
Deardorff, J. W. (1976),On the entrainment rate of a strato-cumulus-topped mixed layer, Q. J. R. Meteorol. Soc.102, 563–582.
Elsasser, W. M. andCulbertson, M. F. (1960),Atmospheric radiation tables, Meteor. Monog.4, 1–43.
Emmons, G. andMontgomery, R. B. (1947),Note on the physics of fog formation, J. Meteorol.4, 206.
Fels, S. B. andKaplan, L. D. (1975),A test of the role of longwave radiative transfer in a general circulation model, J. Atmos. Sci.32, 779–789.
Grassl, H. (1976),A new type of absorption in the atmospheric infrared window due to water vapor polymers, Beit Phys. Atmos.49, 225–236.
Howard, J. N., Burch, D. E. andWilliams, D. (1956),Infrared transmission of synthetic atmospheres. IV. Application of theoretical band models, J. Opt. Soc. Am.46, 334–338.
Irvine, W. M. andPollack, J. B. (1968),Infrared optical properties of water and ice spheres, Icarus8, 324–360.
Manton, M. J. (1978),A finite element model of a moist atmospheric boundary layer: Part II-Method of solution, Tellus (in press).
Rodgers, C. D. andWalshaw, C. D. (1966),The computation of infra-red cooling rate in planetary atmospheres, Q. J. R. Meterol. Soc.92, 67–92.
Rodhe, B. (1962),The effect of turbulence on fog formation, Tellus14, 49–86.
Sasamori, T. (1968),The radiative cooling calculation for application to general circulation experiments, J. Appl Meteorol.7, 721–729.
Sasamori, T. (1972),A linear harmonic analysis of atmospheric motion with radiative dissipation. J. Meteorol. Soc. Japan50, 505–517.
Sommeria, G. (1976),Three-dimensional simulation of turbulent processes in an undisturbed trade wind boundary layer, J. Atmos. Sci.33, 216–241.
Yamamoto, G., Tanaka, M. andAsano, S. (1971),Radiative heat transfer in water clouds by infrared radiation, J. Q. Spectrosc. Radiat. Transfer11, 697–708.
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Manton, M.J. Some effects of intra-red radiation on the dynamics of the atmospheric boundary layer. PAGEOPH 116, 1030–1048 (1978). https://doi.org/10.1007/BF00874669
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DOI: https://doi.org/10.1007/BF00874669