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AGU: Geophysical Research Letters

 

Index Terms

  • Atmospheric Composition and Structure: Aerosols and particles
  • Atmospheric Composition and Structure: Cloud physics and chemistry
  • Atmospheric Composition and Structure: Pollution: urban and regional
  • Atmospheric Composition and Structure: Troposphere: composition and chemistry
  • Atmospheric Composition and Structure: Troposphere: constituent transport and chemistry

Abstract

Springtime cloud condensation nuclei concentrations on the west coast of Korea

Seong Soo Yum

Department of Atmospheric Sciences, Yonsei University, Seoul, Korea

James G. Hudson

Division of Atmospheric Sciences, Desert Research Institute, Reno, Nevada, USA

Keun Yong Song

Department of Atmospheric Sciences, Yonsei University, Seoul, Korea

Byoung-Cheol Choi

Korea Global Atmosphere Watch Observatory, Korea Meteorological Administration, Chungnam, Korea

Cloud condensation nuclei (CCN) measurements were made with the Desert Research Institute (DRI) instantaneous CCN spectrometer at the Korea Global Atmosphere Watch (GAW) Observatory (KGAWO) (36°32′N, 126°19′E) on the west coast of the Korean Peninsula from May 1–22, 2004. A TSI CPC3010 counter simultaneously measured condensation nuclei (CN). For seven of these days, submicron aerosol size distributions were also measured with an SMPS. Data were classified maritime or continental according to air mass back trajectories. Average maritime and continental CCN concentrations at 1% supersaturation were 2406 cm−3 and 5292 cm−3, respectively, while CN concentrations were 3983 cm−3 and 8313 cm−3, respectively. The average ratios of CCN to CN concentrations were 0.64 for both maritime and continental. These results suggest ubiquitously high aerosol concentrations in this area regardless of air mass origin.

Received 4 February 2005; accepted 11 April 2005; published 14 May 2005.

Citation: Yum, S. S., J. G. Hudson, K. Y. Song, and B.-C. Choi (2005), Springtime cloud condensation nuclei concentrations on the west coast of Korea, Geophys. Res. Lett., 32, L09814, doi:10.1029/2005GL022641.

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