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An annual cycle of size-resolved aerosol hygroscopicity at a forested site in Colorado
by
Kreidenweis, S. M.
, DeMott, P. J.
, Sullivan, R. C.
, Ortega, J.
, Prenni, A. J.
, Levin, E. J. T.
, Petters, M. D.
, Atwood, S. A.
, Smith, J. N.
in
aerosol
/ Aerosols
/ Air sampling
/ Atmospheric aerosols
/ Atmospheric sciences
/ biogenic aerosol
/ CCN
/ Chemistry
/ Clouds
/ Earth sciences
/ Earth, ocean, space
/ Exact sciences and technology
/ Geophysics
/ Hydrologic cycle
/ hygroscopicity
/ Organic compounds
/ Physics
/ Seasonal variations
/ Summer
/ Supersaturation
2012
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An annual cycle of size-resolved aerosol hygroscopicity at a forested site in Colorado
by
Kreidenweis, S. M.
, DeMott, P. J.
, Sullivan, R. C.
, Ortega, J.
, Prenni, A. J.
, Levin, E. J. T.
, Petters, M. D.
, Atwood, S. A.
, Smith, J. N.
in
aerosol
/ Aerosols
/ Air sampling
/ Atmospheric aerosols
/ Atmospheric sciences
/ biogenic aerosol
/ CCN
/ Chemistry
/ Clouds
/ Earth sciences
/ Earth, ocean, space
/ Exact sciences and technology
/ Geophysics
/ Hydrologic cycle
/ hygroscopicity
/ Organic compounds
/ Physics
/ Seasonal variations
/ Summer
/ Supersaturation
2012
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An annual cycle of size-resolved aerosol hygroscopicity at a forested site in Colorado
by
Kreidenweis, S. M.
, DeMott, P. J.
, Sullivan, R. C.
, Ortega, J.
, Prenni, A. J.
, Levin, E. J. T.
, Petters, M. D.
, Atwood, S. A.
, Smith, J. N.
in
aerosol
/ Aerosols
/ Air sampling
/ Atmospheric aerosols
/ Atmospheric sciences
/ biogenic aerosol
/ CCN
/ Chemistry
/ Clouds
/ Earth sciences
/ Earth, ocean, space
/ Exact sciences and technology
/ Geophysics
/ Hydrologic cycle
/ hygroscopicity
/ Organic compounds
/ Physics
/ Seasonal variations
/ Summer
/ Supersaturation
2012
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An annual cycle of size-resolved aerosol hygroscopicity at a forested site in Colorado
Journal Article
An annual cycle of size-resolved aerosol hygroscopicity at a forested site in Colorado
2012
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Overview
The ability of particles composed wholly or partially of biogenic secondary organic compounds to serve as cloud condensation nuclei (CCN) is a key characteristic that helps to define their roles in linking biogeochemical and water cycles. In this paper, we describe size‐resolved (14–350 nm) CCN measurements from the Manitou Experimental Forest in Colorado, where particle compositions were expected to have a large biogenic component. These measurements were conducted for 1 year as part of the Bio‐hydro‐atmosphere Interactions of Energy, Aerosols, Carbon, H2O, Organics, and Nitrogen program and determined the aerosol hygroscopicity parameter, κ, at five water supersaturations between ∼0.14% and ∼0.97%. The average κ value over the entire study and all supersaturations was κavg = 0.16 ± 0.08. Kappa values decreased slightly with increasing supersaturation, suggesting a change in aerosol composition with dry diameter. Furthermore, some seasonal variability was observed with increased CCN concentrations and activated particle number fraction, but slightly decreased hygroscopicity, during the summer. Small particle events, which may indicate new particle formation, were observed throughout the study period, especially in the summer, leading to increases in CCN concentration, followed by a gradual increase in the aerosol mode size. The condensing material appeared to be predominantly composed of organic compounds and led to a small decrease in κ at the larger activation diameters during and immediately after those events. Key Points Organic aerosols are an important link in biohydroatmosphere interactions Aerosol hygroscopicity at the BEACHON site indicates a high organic fraction New particle formation can increase CCN concentration but decrease hygroscopicity
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