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CCN-supersaturation spectra slopes (k)Theoretically the slope k of a CCN-supesaturation spectrum should equal two thirds of the slope of the total (soluble) aerosol size distribution. Workshop results tended to verify this relation. The k values are markedly different depending on whether one is measuring ambient CCN concentrations at supersaturations S above or below approximately 0.1-0.2%. The larger k values for S approximately 0.1% is consistent with the greater decrease in large particle concentration with increasing size. It is concluded that over the S range of 0.02% to 2%, two power fits (and k values) may sometimes suffice for a reasonable approximation of the CCN distribution. At other times, and with laboratory generated aeosols, such an approach is inadequate and requires refinement.
Document ID
19820007527
Acquisition Source
Legacy CDMS
Document Type
Conference Paper
Authors
Jiusto, J. E.
(State Univ. of New York Albany, NY, United States)
Lala, G. G.
(State Univ. of New York Albany, NY, United States)
Date Acquired
August 10, 2013
Publication Date
November 1, 1981
Publication Information
Publication: Desert Research Inst. The Third Intern. Cloud Condensation Nuclei Workshop
Subject Category
Instrumentation And Photography
Accession Number
82N15400
Funding Number(s)
CONTRACT_GRANT: NSF ATM-76-24048-02
CONTRACT_GRANT: DAAG29-81-K-0019
Distribution Limits
Public
Copyright
Work of the US Gov. Public Use Permitted.
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