Hygroscopic chemicals and the formation of advection warm fog : A numerical simulation
- Author:
- Liaw, G. S.
- Published:
- Dec 1, 1978.
- Physical Description:
- 1 electronic document
- Additional Creators:
- Hung, R. J.
Online Version
- hdl.handle.net , Connect to this object online.
- Restrictions on Access:
- Unclassified, Unlimited, Publicly available.
Free-to-read Unrestricted online access - Summary:
- The formation of advection fog is closely associated with the characteristics of the aerosol particles, including the chemical composition, mass of the nuclei, particle size, and concentration. Both macrophysical and microphysical processes are considered. In the macrophysical model, the evolution of wind components, water vapor content, liquid water content and potential temperature under the influences of vertical turbulent diffusion, turbulent momentum, and turbulent energy transfers are taken into account. In the microphysical model, the supersaturation effect is incorporated with the surface tension and hygroscopic material solution.
- Other Subject(s):
- Collection:
- NASA Technical Reports Server (NTRS) Collection.
- Note:
- Document ID: 19790006506.
Accession ID: 79N14677.
NASA-CR-3085.
M-278. - Terms of Use and Reproduction:
- No Copyright.
View MARC record | catkey: 15726870