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COMPUTATION OF THE EXTINCTION OF VISIBLE RADIATION BY ATMOSPHERIC AEROSOL PARTICLES AS A FUNCTION OF THE RELATIVE HUMIDITY, BASED UPON MEASURED PROPERTIESHAENEL G.1972; J. AEROSOL SCI.,; G.B.; DA. 1972; VOL. 3; NO 5; PP. 377-386; BIBL. 17REF.Serial Issue

PREDICTION OF THE STANDARD VISUAL RANGE AT HIGH RELATIVE HUMIDITY: A SUMMARY CONSIDERING RECENT DATAHAENEL G.1980; BEITR. PHYS. ATMOS.; ISSN 0005-8173; DEU; DA. 1980; VOL. 53; NO 4; PP. 539-541; ABS. GER; BIBL. 10 REF.Article

AMEISEN, KOMPOST, PFLANZENERZIEHUNG OHNE GIFT = FOURMIS, COMPOST, PEPINIERES SANS PRODUITS TOXIQUESHAENEL G.1979; WALDHYGIENE; DEU; DA. 1979; VOL. 13; NO 1; PP. 11-12Article

THE RATIO OF THE EXTINCTION COEFFICIENT TO THE MASS OF ATMOSPHERIC AEROSOL PARTICLES AS A FUNCTION OF THE RELATIVE HUMIDITYHAENEL G.1972; J. AEROSOL SCI.; G.B.; DA. 1972; VOL. 3; NO 6; PP. 455-460; H.T. 1; BIBL. 5REF.Serial Issue

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