Observations of the evolution of the aerosol, cloud and boundary-layer characteristics during the 1st ACE-2 Lagrangian experiment

Doug W. Johnson, Simon Osborne, Robert Wood, Karsten Suhre, Patricia K. Quinn, Tim Bates, M. O. Andreae, Kevin J. Noone, Paul Glantz, Brian Bandy, J. Rudolph, Colin O'Dowd

Research output: Contribution to journalArticle

28 Citations (Scopus)

Abstract

During the 1st Lagrangian experiment of the North Atlantic Regional Aerosol Characterisation Experiment (ACE-2), a parcel of air was tagged by releasing a smart, constant level balloon into it from the Research Vessel Vodyanitskiy. The Meteorological Research Flight's C-130 aircraft then followed this parcel over a period of 30 h characterising the marine boundary layer (MBL), the cloud and the physical and chemical aerosol evolution. The air mass had originated over the northern North Atlantic and thus was clean and had low aerosol concentrations. At the beginning of the experiment the MBL was over 1500 m deep and made up of a surface mixed layer (SML) underlying a layer containing cloud beneath a subsidence inversion. Subsidence in the free troposphere caused the depth of the MBL to almost halve during the experiment and, after 26 h, the MBL became well mixed throughout its whole depth. Salt particle mass in the MBL increased as the surface wind speed increased from 8 m s-1 to 16 m s-1 and the accumulation mode (0.1 μm to 3.0 μm) aerosol concentrations quadrupled from 50 cm-3 to 200 cm-3. However, at the same time the total condensation nuclei (>3 nm) decreased from over 1000 cm-3 to 750 cm-3. The changes in the accumulation mode aerosol concentrations had a significant effect on the observed cloud microphysics. Observational evidence suggests that the important processes in controlling the Aitken mode concentration which, dominated the total CN concentration, included, scavenging of interstitial aerosol by cloud droplets, enhanced coagulation of Aitken mode aerosol and accumulation mode aerosol due to the increased sea salt aerosol surface area, and dilution of the MBL by free tropospheric air.

Original languageEnglish
Pages (from-to)348-374
Number of pages27
JournalTellus, Series B: Chemical and Physical Meteorology
Volume52
Issue number2
Publication statusPublished - Apr 2000
Externally publishedYes

Fingerprint

ACE 2
volcanic cloud
boundary layer
aerosol
experiment
subsidence
cloud microphysics
research vessel
cloud droplet
air
sea salt
surface wind
coagulation
air mass
mixed layer
condensation
surface layer
troposphere
aircraft
dilution

ASJC Scopus subject areas

  • Atmospheric Science

Cite this

Observations of the evolution of the aerosol, cloud and boundary-layer characteristics during the 1st ACE-2 Lagrangian experiment. / Johnson, Doug W.; Osborne, Simon; Wood, Robert; Suhre, Karsten; Quinn, Patricia K.; Bates, Tim; Andreae, M. O.; Noone, Kevin J.; Glantz, Paul; Bandy, Brian; Rudolph, J.; O'Dowd, Colin.

In: Tellus, Series B: Chemical and Physical Meteorology, Vol. 52, No. 2, 04.2000, p. 348-374.

Research output: Contribution to journalArticle

Johnson, DW, Osborne, S, Wood, R, Suhre, K, Quinn, PK, Bates, T, Andreae, MO, Noone, KJ, Glantz, P, Bandy, B, Rudolph, J & O'Dowd, C 2000, 'Observations of the evolution of the aerosol, cloud and boundary-layer characteristics during the 1st ACE-2 Lagrangian experiment', Tellus, Series B: Chemical and Physical Meteorology, vol. 52, no. 2, pp. 348-374.
Johnson, Doug W. ; Osborne, Simon ; Wood, Robert ; Suhre, Karsten ; Quinn, Patricia K. ; Bates, Tim ; Andreae, M. O. ; Noone, Kevin J. ; Glantz, Paul ; Bandy, Brian ; Rudolph, J. ; O'Dowd, Colin. / Observations of the evolution of the aerosol, cloud and boundary-layer characteristics during the 1st ACE-2 Lagrangian experiment. In: Tellus, Series B: Chemical and Physical Meteorology. 2000 ; Vol. 52, No. 2. pp. 348-374.
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