6533b85ffe1ef96bd12c1bac
RESEARCH PRODUCT
Visibility forecast in the phase of pre-condensation
Fritz Kastensubject
PhysicsAtmospheric Science010504 meteorology & atmospheric sciencesbusiness.industryCondensationVisibility (geometry)Phase (waves)Analytical chemistryHumidityGeneral MedicineOceanography01 natural sciencesAerosolOpticsVisual rangeExponentRelative humiditybusiness0105 earth and related environmental sciencesdescription
The effect on visibility of the swelling of aerosol particles due to increasing humidity is studied. The swelling can be described by r(f)/r (0) = (1 - f ) ?1/? where r ( f ) = particle radius at relative humidity f and ? = const ? 4 on the average. The visibility variation is expressed as V(f)/V(f 0 ) = [(1 - f )/(1 - f 0 )] V * ? 1)/? where V * = exponent of the aerosol size distribution ? 3 on the average. The last formula allows to compute the standard visual range V(f) at relative humidity f from the present standard visual range V(f 0 ) at present relative humidity f 0 . DOI: 10.1111/j.2153-3490.1969.tb00469.x
year | journal | country | edition | language |
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1969-10-01 | Tellus A: Dynamic Meteorology and Oceanography |