Balloon observations of nitric acid aerosol formation in the arctic stratosphere. I - Gaseous nitric acid. II - Aerosol

Computer Science – Sound

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Aerosols, Arctic Regions, Balloon Sounding, Nitric Acid, Ozone Depletion, Stratosphere, Atmospheric Chemistry, Low Temperature Tests, Mass Spectrometers, Pressure Distribution, Temperature Profiles, Vertical Distribution

Scientific paper

A case study of nitric acid trihydrate (NAT) aerosol formation in the winter arctic stratosphere using balloon-borne measurements of gaseous nitric acid and aerosols is presented. The measurements were made under very low stratospheric temperature conditions, with minimum values of 186 K at about 24 km altitude, being approximately six degrees less than the existence temperature T(NAT) for NAT aerosols. It is concluded from these data that rapid formation of NAT-aerosols associated with substantial condensational depletion of gaseous nitric acid occurred only at temperatures of approximately three to four degrees below T(NAT) corresponding to large HNO3-supersaturations, which are probably required for activation of a major fraction of preexisting condensation nuclei. Also balloon-borne aerosol measurements over the size range r = 0.01 to 10 microns on January 31, 1990 were used to determine the HNO3 vapor mass deposited in Arctic NAT clouds in the 21-24 km region. Results indicate that the maximum inferred HNO3 vapor mixing ratio that condensed in the cloud was approximately 4 ppbv, in good agreement with the observed depletion of HNO3 vapor in the same altitude region under like temperature conditions 23 hours earlier.

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