Parametrization of the ice‐phase in a model of mid‐latitude cumulonimbus convection and its influence on the simulation of cloud development | Zendy

Bennetts D. A. | Zendy; Rawlins F. | Zendy

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Parametrization of the ice‐phase in a model of mid‐latitude cumulonimbus convection and its influence on the simulation of cloud development

Author(s) -

Bennetts D. A.,

Rawlins F.

Publication year - 1981

Publication title -

quarterly journal of the royal meteorological society

Language(s) - English

Resource type - Journals

SCImago Journal Rank - 1.744

H-Index - 143

eISSN - 1477-870X

pISSN - 0035-9009

DOI - 10.1002/qj.49710745302

Subject(s) - parametrization (atmospheric modeling) , cloud computing , precipitation , meteorology , convection , storm , atmospheric sciences , climatology , geology , environmental science , physics , computer science , quantum mechanics , operating system , radiative transfer

The three‐dimensional model of deep tropical convection described in Miller and Pearce (1974) has been extended by the incorporation of a parametrized ice phase. This parametrization is capable of describing two routes for the formation of precipitation, cloud water → cloud ice→hail and cloud water→rain→ hail, and these are investigated separately, Numerical simulations are then compared with an observational study of two cumulonimbi, one a single‐celled cloud and the other a multi‐celled storm. Special attention is paid to the growth of a daughter cell on one flank.

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