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Analysis of the physical state of one Arctic polar stratospheric cloud based on observationsDuring the Arctic Airborne Stratospheric Expedition (AASE) simultaneous measurements of aerosol size distribution and NO(y)(HN03 + NO + NO2 + 2(N205)) were made along ER-2 flight paths. The flow characteristics of the NO(y) instrument allow us to derive the condensed NO(y) amount (assumed to be HN03) present during polar stratospheric cloud (PSC) events. Analysis of the January 24th flight indicates that this condensed HN03 amount does not agree well with the aerosol volume if the observed PSCs are composed of solid nitric acid trihydrate (NAT), as is generally assumed. However, the composition agrees well with that predicted for liquid H2S04/HN03/H20 solution droplets using a new Aerosol Physical Chemistry Model (APCM). The agreement corresponds in detail to variations in temperature and humidity. The weight percentages of H2SO4, HN03, and H2O derived from the measurements all correspond to those predicted for ternary, liquid solutions.
Document ID
19950046383
Acquisition Source
Legacy CDMS
Document Type
Reprint (Version printed in journal)
External Source(s)
Authors
Drdla, K.
(Univ. of California at Los Angeles, Los Angeles, CA United States)
Tabazadeh, A.
(NASA Ames Research Center Moffett Field, CA, United States)
Turco, R. P.
(Univ. of California at Los Angeles, Los Angeles, CA United States)
Jacobson, M. Z.
(Univ. of California at Los Angeles, Los Angeles, CA United States)
Dye, J. E.
(National Center for Atmospheric Research, Boulder, CO United States)
Twohy, C.
(National Center for Atmospheric Research, Boulder, CO United States)
Baumgardner, D.
(National Center for Atmospheric Research, Boulder, CO United States)
Date Acquired
August 16, 2013
Publication Date
November 15, 1994
Publication Information
Publication: Geophysical Research Letters
Volume: 21
Issue: 23
ISSN: 0094-8276
Subject Category
Geophysics
Accession Number
95A77982
Funding Number(s)
CONTRACT_GRANT: NAGW-2183
Distribution Limits
Public
Copyright
Other

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