ISSN:
0928-5105
Source:
Springer Online Journal Archives 1860-2000
Topics:
Geosciences
,
Physics
Notes:
Abstract Based on an experimental study of directed dissipation coefficients and aerosol microstructure in the coastal area the problem of wind regime manifestation is considered. It is shown that the main changes of parameters of dissipation indicatrix form near angles ϕ=15°–165°, which are conditioned by submicron fractions of aerosol particles, take place without regard for wind regime. Usually they are defined by effect of relative air humidity. It is found that specific manifestations of wind regime are observed close to small dissipation angles and are conditioned by the effect of coarse-dispersed aerosol fractions.
Type of Medium:
Electronic Resource
URL:
http://dx.doi.org/10.1007/BF02198289
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