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On the vertical velocity at the top of the planetary boundary layer in nonstationary conditions

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Abstract

The non-stationary planetary boundary layer is parameterized for use in weather forecasting numerical models.

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Reference

  • Kazanskii, A. B. and Monin, A. S.: 1961, ‘On the Dynamical Interaction Between the Atmosphere and Earth's Surface’, Izv. Akad. Nauk, Ser. Geophys. 5, 786–788; Engl. transl. 514–515.

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Authors and Affiliations

  1. Hydrometeorological Institute, Leningrad, U.S.S.R.

    D. L. Laikhtman

  2. Geophysical Institute, Bulgarian Academy of Sciences, Sofia, Bulgaria

    D. L. Yordanov

Authors
  1. D. L. Laikhtman
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  2. D. L. Yordanov
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Laikhtman, D.L., Yordanov, D.L. On the vertical velocity at the top of the planetary boundary layer in nonstationary conditions. Boundary-Layer Meteorol 17, 293–296 (1979). https://doi.org/10.1007/BF00117920

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  • DOI: https://doi.org/10.1007/BF00117920

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