Work

Extension of the Stochastic Mixing Model to Cumulonimbus Clouds

Year: 1992

Type: article

Abstract: The stochastic mixing model of cumulus clouds is extended to the case in which ice and precipitation form. A simple cloud microphysical model is adopted in which ice crystals and aggregates are carried along with the updraft, whereas raindrops, graupel, and hail are assumed to immediately fall out. The model is then applied to the 2 August 1984 case study of convection over the Magdalena Mountains of central New Mexico, with excellent results. The formation of ice and precipitation can explain the transition of this system from a cumulus congestus cloud to a thunderstorm.

Source: Journal of the Atmospheric Sciences

DOI: 10.1175/1520-0469(1992)049<1968:eotsmm>2.0.co;2

Authors: D. J. Raymond, A. M. Blyth

Institution: New Mexico Institute of Mining and Technology

Language: English

Topic: Meteorological Phenomena and Simulations

Subfield: Atmospheric Science

Field: Earth and Planetary Sciences

Domain: Physical Sciences

Open Access status: bronze

OpenAlex ID: W1984843597

FWCI: 0.934

Cites:

Cited by: 82

Related to: 10