Airborne measurements of nucleation mode particles I: coastal nucleation and growth rates

被引:35
作者
O'Dowd, C. D.
Yoon, Y. J.
Junkerman, W.
Aalto, P.
Kulmala, M.
Lihavainen, H.
Viisanen, Y.
机构
[1] Natl Univ Ireland Univ Coll Galway, Dept Phys & Environm, Change Inst, Galway, Ireland
[2] KORDI, Korea Polar Res Inst, Inchon 406840, South Korea
[3] Fraunhofer Inst Atmosphar Umweltforsch, D-82467 Garmisch Partenkirchen, Germany
[4] Univ Helsinki, Dept Phys Sci, FIN-00014 Helsinki, Finland
[5] Finnish Meteorol Inst, Erik Palmenin Aukio, FIN-00101 Helsinki, Finland
关键词
D O I
10.5194/acp-7-1491-2007
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
A light aircraft was equipped with a bank of Condensation Particle Counters (CPCs) (50% cut from 3-5.4-9.6 nm) and a nano-Scanning Mobility Particle Sizer (nSMPS) and deployed along the west coast of Ireland, in the vicinity of Mace Head. The objective of the exercise was to provide high resolution micro-physical measurements of the coastal nucleation mode in order to map the spatial extent of new particle production regions and to evaluate the evolution, and associated growth rates of the coastal nucleation-mode aerosol plume. Results indicate that coastal new particle production is occurring over most areas along the land-sea interface with peak concentrations at the coastal plume-head in excess of 10(6) cm(-3). Pseudo-Lagrangian studies of the coastal plume evolution illustrated significant growth of new particles to sizes in excess of 8 nm approximately 10 km downwind of the source region. Close to the plume head (<1 km) growth rates can be as high as 123-171 nm h(-1), decreasing gradually to 53-72 nm h(-1) at 3 km. Further along the plume, at distances up to 10 km, the growth rates are calculated to be 17-32 nm h(-1). Growth rates of this magnitude suggest that after a couple of hours, coastal nucleation mode particles can reach significant sizes where they can contribution to the regional aerosol loading.
引用
收藏
页码:1491 / 1501
页数:11
相关论文
共 25 条
[1]   Physical characterization of aerosol particles during nucleation events [J].
Aalto, P ;
Hämeri, K ;
Becker, E ;
Weber, R ;
Salm, J ;
Mäkelä, JM ;
Hoell, C ;
O'Dowd, CD ;
Karlsson, H ;
Hansson, HC ;
Väkevä, M ;
Koponen, IK ;
Buzorius, G ;
Kulmala, M .
TELLUS SERIES B-CHEMICAL AND PHYSICAL METEOROLOGY, 2001, 53 (04) :344-358
[2]  
AITKEN JA, 1897, T R SOC EDINBURGH, V39
[3]  
BIRMILI W, 2001, J AEROSOL SCI, V32, pS193
[4]   OCEANIC PHYTOPLANKTON, ATMOSPHERIC SULFUR, CLOUD ALBEDO AND CLIMATE [J].
CHARLSON, RJ ;
LOVELOCK, JE ;
ANDREAE, MO ;
WARREN, SG .
NATURE, 1987, 326 (6114) :655-661
[5]   Particle nucleation in the tropical boundary layer and its coupling to marine sulfur sources [J].
Clarke, AD ;
Davis, D ;
Kapustin, VN ;
Eisele, F ;
Chen, G ;
Paluch, I ;
Lenschow, D ;
Bandy, AR ;
Thornton, D ;
Moore, K ;
Mauldin, L ;
Tanner, D ;
Litchy, M ;
Carroll, MA ;
Collins, J ;
Albercook, C .
SCIENCE, 1998, 282 (5386) :89-92
[6]   Condensation and coagulation sinks and formation of nucleation mode particles in coastal and boreal forest boundary layers -: art. no. 8097 [J].
Dal Maso, M ;
Kulmala, M ;
Lehtinen, KEJ ;
Mäkelä, JM ;
Aalto, P ;
O'Dowd, CD .
JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES, 2002, 107 (D15)
[7]  
Draxler R.R., 2010, HYSPLIT HYBRID SINGL
[8]  
[Houghton J.T. IPCC. IPCC.], 2001, CLIMATE CHANGE
[9]   SIZE DISTRIBUTION OF ANTARCTIC SUBMICRON AEROSOLS [J].
ITO, T .
TELLUS SERIES B-CHEMICAL AND PHYSICAL METEOROLOGY, 1993, 45 (02) :145-159
[10]   Initial steps of aerosol growth [J].
Kulmala, M ;
Laakso, L ;
Lehtinen, KEJ ;
Riipinen, I ;
Dal Maso, M ;
Anttila, T ;
Kerminen, VM ;
Horrak, U ;
Vana, M ;
Tammet, H .
ATMOSPHERIC CHEMISTRY AND PHYSICS, 2004, 4 :2553-2560