Numerical model for convective cloud dynamics, microphysics, and photochemistry

Citation
Il. Karol' et al., Numerical model for convective cloud dynamics, microphysics, and photochemistry, IZV ATM O P, 36(6), 2000, pp. 715-729
Citations number
36
Categorie Soggetti
Earth Sciences
Journal title
IZVESTIYA ATMOSPHERIC AND OCEANIC PHYSICS
ISSN journal
00014338 → ACNP
Volume
36
Issue
6
Year of publication
2000
Pages
715 - 729
Database
ISI
SICI code
0001-4338(200011/12)36:6<715:NMFCCD>2.0.ZU;2-5
Abstract
A numerical model for a drop convective cloud with detailed microphysics, c hemistry, and radiation is presented. The condensation and coagulation proc esses are described with the help of a kinetic equation. The coagulation is calculated using a modification of the well-known Kowetz-Alund method. The chemical model includes about 150 gas-phase reactions (with a detailed des cription of transformations in the oxygen, nitrogen, hydrogen, chlorine, su lfur, methane, and ethane cycles) and about 110 aqueous-phase reactions (in cluding both the interphase and aqueous-phase steady-state reactions) that account for diffusion and gas absorption on the cloud drop surfaces. The ph otodissociation rates in the radiative transfer module are calculated using the delta-Eddington scheme. The results of numerical experiments indicate that convective clouds in the troposphere tend to decrease the concentratio ns of highly soluble species due to their capture by the cloud drops and fu rther precipitation scavenging. The vertical transport in convective clouds significantly affects the concentrations of slightly soluble gases. The ra diative processes in clouds have a profound impact on the concentrations of short-lived gaseous species. It is also shown that the aqueous-phase chemi stry calculations must include not only the chemical reactions but also the species redistribution over drop sizes during condensation-evaporation and coagulation processes.